paleo data:
  measurement table:
    table name: paleo1measurement1
    uncertainty low:
      t sid: lcRo2jHvsy5I2rJpCa2
      variable name: uncertaintyLow
      units: yr BP
      primary timeseries: FALSE
      primary age column: false
      summary statistic: min
      datum: 1950
      inferred material: age
      is primary: false
      notes: NA; paleoData_inferredMaterial has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
      median res12k: 140
      mean value12k: 4876.1429
      values: -120
      values: -70
      values: -10
      values: 0
      values: 70
      values: 150
      values: 180
      values: 270
      values: 380
      values: 420
      values: 490
      values: 600
      values: 710
      values: 980
      values: 1250
      values: 1310
      values: 1380
      values: 1450
      values: 1560
      values: 1680
      values: 1770
      values: 1910
      values: 2030
      values: 2260
      values: 2590
      values: 2890
      values: 3260
      values: 3630
      values: 3780
      values: 4080
      values: 4380
      values: 4720
      values: 4890
      values: 5080
      values: 5180
      values: 5300
      values: 5370
      values: 5460
      values: 5530
      values: 5620
      values: 5720
      values: 5800
      values: 5900
      values: 6010
      values: 6120
      values: 6220
      values: 6330
      values: 6440
      values: 6550
      values: 6680
      values: 6930
      values: 7210
      values: 7840
      values: 8220
      values: 8350
      values: 8470
      values: 8600
      values: 8720
      values: 8850
      values: 8990
      values: 9130
      values: 9420
      values: 9730
      values: 10050
      values: 10390
      values: 10760
      values: 11000
      values: 11230
    uncertainty high:
      t sid: lcRJR6bzPuJFl2ftWoi
      variable name: uncertaintyHigh
      units: yr BP
      primary timeseries: FALSE
      primary age column: false
      summary statistic: max
      datum: 1950
      is primary: false
      notes: NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
      median res12k: 140
      mean value12k: 5529.8571
      values: 60
      values: 270
      values: 430
      values: 530
      values: 640
      values: 740
      values: 820
      values: 920
      values: 1000
      values: 1060
      values: 1090
      values: 1180
      values: 1250
      values: 1320
      values: 1400
      values: 1730
      values: 1950
      values: 2140
      values: 2340
      values: 2520
      values: 2650
      values: 2840
      values: 2980
      values: 3220
      values: 3530
      values: 3750
      values: 3960
      values: 4130
      values: 4340
      values: 4690
      values: 4990
      values: 5280
      values: 5420
      values: 5540
      values: 5610
      values: 5660
      values: 5850
      values: 6050
      values: 6210
      values: 6360
      values: 6510
      values: 6640
      values: 6770
      values: 6900
      values: 7050
      values: 7170
      values: 7280
      values: 7380
      values: 7490
      values: 7630
      values: 7840
      values: 8050
      values: 8400
      values: 8540
      values: 8780
      values: 8990
      values: 9180
      values: 9350
      values: 9530
      values: 9700
      values: 9870
      values: 10170
      values: 10460
      values: 10740
      values: 11000
      values: 11250
      values: 11560
      values: 11860
      values: 12140
    age:
      t sid: lcR6Zf0IQfOhT3ICqCB
      variable name: age
      units: yr BP
      primary timeseries: false
      primary age column: true
      summary statistic: median
      datum: 1950
      is primary: true
      notes: NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
      values: -40
      values: 50
      values: 160
      values: 210
      values: 320
      values: 420
      values: 480
      values: 590
      values: 710
      values: 770
      values: 820
      values: 930
      values: 1050
      values: 1210
      values: 1320
      values: 1440
      values: 1580
      values: 1730
      values: 1890
      values: 2050
      values: 2170
      values: 2340
      values: 2490
      values: 2740
      values: 3090
      values: 3370
      values: 3690
      values: 3970
      values: 4110
      values: 4400
      values: 4700
      values: 5010
      values: 5160
      values: 5300
      values: 5370
      values: 5440
      values: 5540
      values: 5680
      values: 5800
      values: 5930
      values: 6060
      values: 6180
      values: 6290
      values: 6420
      values: 6560
      values: 6680
      values: 6790
      values: 6910
      values: 7040
      values: 7180
      values: 7420
      values: 7680
      values: 8180
      values: 8410
      values: 8570
      values: 8710
      values: 8870
      values: 9020
      values: 9180
      values: 9330
      values: 9480
      values: 9800
      values: 10110
      values: 10410
      values: 10720
      values: 11030
      values: 11270
      values: 11510
      values: 11760
      values: 11990
      values: 12380
archive type: LakeSediment
data set name: LittleWilleyPond.Oswald.2018
dataset id: LC05e62b47aeb15762ec0d23f3ce79dc95
created by: github.com/nickmckay/LegacyClimate2LiPD
original data source: Neotoma
legacy climate site id: 23693
legacy climate dataset id: 40992
ages per kyr: NA
max year: 13130
min year: -40
original data url: https://doi.org/10.1594/10.1594/PANGAEA.930512
lipdverse link: https://lipdverse.org/data/LC05e62b47aeb15762ec0d23f3ce79dc95/1_0_7
lipd version: 1.3
dataset version: 1.0.7
pub: Subregional variability in the response of New England vegetation to postglacial climate change.

scope: climate

scope: climate

scope: climate
variable: precipitation
variable detail: precipitation@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: WA-PLS
target: all

scope: climate
variable: precipitation
variable detail: precipitation@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: MAT
target: all

scope: climate
variable: precipitation
variable detail: precipitation@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: MAT
target: all

scope: climate
variable: precipitation
variable detail: precipitation@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: WA-PLS
target: July temperature-tailored

scope: climate
variable: precipitation
variable detail: precipitation@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: WA-PLS
target: annual mean temperature-tailored

scope: climate
variable: precipitation
variable detail: amount@surface
seasonality: Annual
direction: positive
seasonality general: Annual

method: WA-PLS
target: annual precipitation-tailored

compilation name: HoloceneHydroclimate
compilation version: 0_6_0
compilation version: 0_7_0
compilation version: 0_8_0
compilation version: 0_9_0
compilation version: 0_9_1

compilation name: HoloceneAbruptChange
compilation version: 0_11_0

t sid: lcRgQ9f7kUUFMjB6DXo
variable name: age
units: yr BP
primary timeseries: false
primary age column: false
summary statistic: mean
datum: 1950
is primary: false
notes: NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
values: -40
values: 60
values: 170
values: 220
values: 320
values: 430
values: 480
values: 600
values: 710
values: 760
values: 810
values: 920
values: 1030
values: 1190
values: 1320
values: 1460
values: 1600
values: 1740
values: 1900
values: 2070
values: 2180
values: 2350
values: 2490
values: 2740
values: 3080
values: 3360
values: 3670
values: 3940
values: 4100
values: 4400
values: 4700
values: 5000
values: 5160
values: 5300
values: 5380
values: 5450
values: 5560
values: 5700
values: 5810
values: 5940
values: 6070
values: 6190
values: 6310
values: 6440
values: 6570
values: 6680
values: 6800
values: 6910
values: 7030
values: 7170
values: 7410
values: 7660
values: 8160
values: 8400
values: 8570
values: 8720
values: 8870
values: 9020
values: 9180
values: 9330
values: 9490
values: 9800
values: 10100
values: 10410
values: 10710
values: 11020
values: 11270
values: 11520
values: 11770
values: 12020
values: 12400

t sid: lcRD0fdGOjxSYe2H9Hp
variable name: depth
units: cm
primary timeseries: false
primary age column: false
summary statistic: mean
is primary: true
notes: NA; paleoData_isPrimary has been standardized
values: 0
values: 4
values: 8
values: 10
values: 14
values: 18
values: 20
values: 24
values: 28
values: 30
values: 32
values: 36
values: 40
values: 46
values: 51
values: 56
values: 61
values: 66
values: 72
values: 78
values: 82
values: 88
values: 93
values: 102
values: 114
values: 124
values: 135
values: 145.5
values: 156
values: 177
values: 198
values: 219
values: 230
values: 240
values: 245
values: 250
values: 255
values: 261
values: 266
values: 271.5
values: 277
values: 282
values: 287
values: 292.5
values: 298
values: 303
values: 308
values: 313
values: 318
values: 324
values: 334.5
values: 345
values: 366
values: 376.5
values: 387
values: 397.5
values: 408
values: 418.5
values: 429
values: 439.5
values: 450
values: 471
values: 492
values: 513
values: 534
values: 555
values: 576
values: 597
values: 618
values: 639
values: 660
values: 680

t sid: lcRYF2YGANynsAsu1hX
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 19.5157
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 20.2
values: 19.6
values: 19.8
values: 18.6
values: 19
values: 18.9
values: 18.7
values: 18.5
values: 18.4
values: 18.3
values: 18.1
values: 18.8
values: 19.2
values: 20
values: 19.3
values: 19.7
values: 19.4
values: 19.9
values: 20.6
values: 20.5
values: 21.2
values: 19.5
values: 20.1
values: 21
values: 20.8
values: 20.3
values: 20.7
values: 19.1
values: 17
values: 16.9
values: 16
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRRfMoSqdPTDda1F8t
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.5706
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.57
values: 1.58
values: 1.59
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRplMkhCiVPIvwDFKV
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 19.5657
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 19.8
values: 19.6
values: 19.2
values: 18.5
values: 18.8
values: 19.1
values: 18.9
values: 18.7
values: 19.4
values: 19.3
values: 19.5
values: 19.7
values: 19.9
values: 20
values: 20.1
values: 20.2
values: 19
values: 18.2
values: 17.6
values: 17.4
values: 14.5
values: 15.5
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcR5HjgKD1wkbXAbn2Y
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.0773
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.07
values: 1.06
values: 1.08
values: 1.09
values: 1.11
values: 1.1
values: 1.05
values: 1.12
values: 1.34
values: 1.47
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcR64AHdbeC6hWUlwYg
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 6.4743
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 7
values: 5.9
values: 6.9
values: 5.3
values: 5.8
values: 6.1
values: 5.5
values: 6
values: 5.4
values: 6.4
values: 5.6
values: 7.9
values: 6.3
values: 6.6
values: 6.5
values: 6.8
values: 7.2
values: 6.7
values: 7.4
values: 7.6
values: 8
values: 7.3
values: 7.1
values: 9.5
values: 8.1
values: 7.5
values: 7.7
values: 5.7
values: 4.5
values: 3.4
values: 3.6
values: 1.6
values: 0.7
values: 0.6
values: 3.7
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRLhHuAeNYsXAxFBep
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.9787
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.97
values: 1.98
values: 1.99
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRTMLOWthm9bcDABcd
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 5.7857
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 6
values: 5.9
values: 5.8
values: 6.1
values: 5.7
values: 5
values: 5.3
values: 5.5
values: 6.4
values: 5.6
values: 6.5
values: 6.2
values: 6.3
values: 4.7
values: 5.4
values: 5.1
values: 4.9
values: 2.2
values: 2.4
values: 2.8
values: 1.6
values: -2.9
values: -2.1
values: 3.8
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcR5IymQT49lQwZoCf1
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.2797
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.28
values: 1.29
values: 1.27
values: 1.3
values: 1.26
values: 1.31
values: 1.32
values: 1.34
values: 1.33
values: 1.47
values: 1.61
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRRjuWEHVRbLBeeRyH
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 1114.1471
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 1042.4
values: 1035.3
values: 1165.4
values: 1103.6
values: 1145.5
values: 1193
values: 1153.8
values: 1229.7
values: 1156.8
values: 1218.9
values: 1237.9
values: 1178.6
values: 1165.1
values: 1140.7
values: 1235.3
values: 1159.3
values: 1174.6
values: 1266.4
values: 1161.7
values: 1173
values: 1139.3
values: 1120.8
values: 1188
values: 1202.9
values: 1182.5
values: 1128.1
values: 1143.6
values: 1167.7
values: 1132.3
values: 1151.5
values: 1169.2
values: 1212.9
values: 1181.4
values: 1135.5
values: 1142
values: 1144.1
values: 1063.8
values: 1131.6
values: 1143.5
values: 1172.8
values: 1256.4
values: 1235.8
values: 1087.9
values: 1173.1
values: 1189.1
values: 1216.4
values: 1208.5
values: 1164.8
values: 1209.8
values: 1105.8
values: 1115.9
values: 1077.6
values: 1013.2
values: 998.6
values: 1012.4
values: 1025.5
values: 976.4
values: 957.2
values: 1032.4
values: 956.1
values: 1023
values: 1006.2
values: 912.8
values: 935.6
values: 974.9
values: 964.7
values: 994.3

t sid: lcRrWZYNBcSErwg5oGa
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 166.7187
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 166.48
values: 166.35
values: 166.44
values: 166.45
values: 166.51
values: 166.6
values: 166.87
values: 166.74
values: 166.84
values: 166.82
values: 166.9
values: 166.81
values: 166.89
values: 166.98
values: 166.86
values: 166.96
values: 167.03
values: 166.79
values: 166.91
values: 166.73
values: 166.93
values: 166.66
values: 166.65
values: 166.57
values: 166.71
values: 166.61
values: 166.69
values: 166.62
values: 166.8
values: 166.92
values: 167.48
values: 166.99
values: 167.36
values: 166.55
values: 166.7
values: 166.46
values: 166.47
values: 166.42
values: 166.56
values: 166.38
values: 166.43
values: 166.58
values: 166.54
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRqfCsEy30NlQfew2H
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 957.3529
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 895.4
values: 928.1
values: 1071.6
values: 1028.6
values: 1037
values: 1098.9
values: 1039.3
values: 1085.7
values: 1065.4
values: 1038.6
values: 1109.6
values: 1065.1
values: 1076.3
values: 1049.8
values: 1072
values: 1028.5
values: 1074.6
values: 1054.9
values: 1016.8
values: 1029.2
values: 1043.6
values: 1096.5
values: 1052
values: 1084
values: 1022
values: 992.3
values: 995.5
values: 933.2
values: 955
values: 1017.4
values: 1064.7
values: 993.4
values: 974.2
values: 974.6
values: 1050.2
values: 987.3
values: 963.8
values: 917.7
values: 996.4
values: 1018.3
values: 1010.6
values: 965.7
values: 982.9
values: 1012.5
values: 975
values: 973.9
values: 979.4
values: 967.6
values: 912.7
values: 935.3
values: 888.7
values: 860.8
values: 798.9
values: 820.4
values: 838.2
values: 780.4
values: 779.8
values: 803.7
values: 782.1
values: 776.5
values: 768
values: 798.3
values: 753.7
values: 770.5
values: 769.7
values: 781.9
values: 805.6

t sid: lcRfribY3hZ5nPLjOXo
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 128.8381
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 128.72
values: 126.17
values: 128.45
values: 123.16
values: 126.01
values: 126.87
values: 123.53
values: 128.13
values: 123.99
values: 121.68
values: 129.68
values: 124.63
values: 126.7
values: 128.51
values: 125.66
values: 129.1
values: 134.76
values: 134.2
values: 135.15
values: 134.46
values: 134.12
values: 132.22
values: 127.77
values: 134.05
values: 128.85
values: 133.67
values: 129.17
values: 126.46
values: 126.33
values: 127.37
values: 130.04
values: 126.45
values: 128
values: 132.59
values: 132.86
values: 132.69
values: 131.61
values: 134.26
values: 136.02
values: 132.64
values: 131.55
values: 136.91
values: 134.4
values: 135.73
values: 139.05
values: 138.87
values: 138.91
values: 129.21
values: 126.34
values: 123.88
values: 122.92
values: 123.87
values: 123.81
values: 122.32
values: 122.34
values: 124.3
values: 123.5
values: 124.77
values: 123.45
values: 123.79
values: 124.17
values: 128.15
values: 124.39
values: 128.57
values: 124.56
values: 125.6

t sid: lcRP188wuX5JZT0dU8X
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 18.9129
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 19.3
values: 19
values: 19.2
values: 18.9
values: 18.7
values: 18.6
values: 18.3
values: 18.8
values: 19.1
values: 19.4
values: 19.5
values: 19.7
values: 19.6
values: 18.2
values: 17.4
values: 17.3
values: 17.5
values: 16.5
values: 17.9
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: July temperature-tailored
in compilation beta:
  compilation name: HoloceneAbruptChange
  compilation version: 0_11_0

t sid: lcR4tKh8R0JknoMiYmG
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 0.96
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 0.96
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: July temperature-tailored

t sid: lcRCyjWNZn4PM2ZBM0H
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 1069.3657
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 981.2
values: 993.7
values: 1152.2
values: 1128.7
values: 1122.4
values: 1186.5
values: 1143.9
values: 1266.9
values: 1159.6
values: 1210.4
values: 1246.6
values: 1197.9
values: 1209.9
values: 1162.8
values: 1261.5
values: 1144.8
values: 1191.3
values: 1219.9
values: 1178.8
values: 1174.4
values: 1139.3
values: 1108
values: 1175.2
values: 1182.7
values: 1161.8
values: 1108.1
values: 1121.4
values: 1131.5
values: 1082.8
values: 1101.8
values: 1106.5
values: 1156.6
values: 1123.1
values: 1079.3
values: 1125.7
values: 1130.7
values: 1050.2
values: 1113.8
values: 1087.2
values: 1137.2
values: 1179.9
values: 1158.2
values: 1066.1
values: 1169.2
values: 1176.4
values: 1180
values: 1166.5
values: 1150.9
values: 1180.4
values: 1031.8
values: 1063.8
values: 1001.4
values: 916.2
values: 922
values: 930.8
values: 938.3
values: 849.8
values: 814.8
values: 919.7
values: 881.6
values: 898.6
values: 881.7
values: 832.1
values: 776.6
values: 838.1
values: 824.4
values: 831.4

t sid: lcRNEoFcKZwZ7McK9z9
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 136.738
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 136.46
values: 136.35
values: 136.76
values: 136.38
values: 136.52
values: 136.47
values: 136.79
values: 136.68
values: 136.81
values: 136.75
values: 136.89
values: 136.92
values: 136.73
values: 136.8
values: 137.09
values: 137
values: 136.71
values: 136.87
values: 136.67
values: 136.91
values: 136.82
values: 136.83
values: 136.63
values: 136.55
values: 136.62
values: 136.53
values: 136.65
values: 136.74
values: 136.61
values: 136.77
values: 137.1
values: 139.37
values: 136.84
values: 136.93
values: 136.9
values: 137.11
values: 139.05
values: 136.45
values: 136.33
values: 136.43
values: 136.42
values: 136.39
values: 136.48
values: 136.4
values: 136.31
values: 136.28
values: 136.6
values: 137.25
values: 137.08
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: July temperature-tailored

t sid: lcRhyCU1d7DO4spNHql
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 5.8186
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 6
values: 5.1
values: 6.4
values: 5.8
values: 5.4
values: 6.2
values: 5.5
values: 6.6
values: 5.7
values: 5.6
values: 6.5
values: 6.1
values: 6.7
values: 7.1
values: 5.9
values: 6.8
values: 6.3
values: 7
values: 8.1
values: 6.9
values: 7.2
values: 7.4
values: 4.9
values: 5
values: 5.3
values: 4.7
values: 4.6
values: 4.5
values: 3.7
values: 4.1
values: 3.6
values: 2.3
values: 2.2
values: 2.1
values: 2
values: 0.6
values: 2.5
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual mean temperature-tailored
in compilation beta:
  compilation name: HoloceneAbruptChange
  compilation version: 0_11_0

t sid: lcRQkS2hE7FLTjylOUy
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.1706
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.17
values: 1.19
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual mean temperature-tailored

t sid: lcRq2fIc4rEaL8HitjN
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 1050.9429
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 963.3
values: 973.7
values: 1146.5
values: 1114.6
values: 1108.8
values: 1181.3
values: 1128.9
values: 1246.3
values: 1143.8
values: 1180.9
values: 1224.5
values: 1177.8
values: 1194.4
values: 1138.7
values: 1232.3
values: 1132.7
values: 1168.4
values: 1193.5
values: 1147.4
values: 1147.7
values: 1115.9
values: 1093.7
values: 1149.2
values: 1158
values: 1136
values: 1084.7
values: 1090.8
values: 1114.7
values: 1058.7
values: 1090.9
values: 1090.6
values: 1146.3
values: 1102.4
values: 1054.4
values: 1108
values: 1113.2
values: 1021.1
values: 1088.8
values: 1066.3
values: 1108.2
values: 1156.6
values: 1118
values: 1034.5
values: 1142.4
values: 1148.7
values: 1146.4
values: 1139.3
values: 1115.5
values: 1151.6
values: 993.7
values: 1040.1
values: 980.8
values: 890.4
values: 901.1
values: 916.9
values: 921.6
values: 837.4
values: 802.4
values: 910.7
values: 873.1
values: 892.9
values: 876.3
values: 826.5
values: 774.2
values: 826.4
values: 825.6
values: 836.1

t sid: lcROSAMWyIx6hXhQsRz
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 142.8543
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 142.48
values: 142.41
values: 142.74
values: 142.43
values: 142.63
values: 142.81
values: 142.66
values: 143
values: 142.86
values: 143.01
values: 142.99
values: 143.04
values: 143.1
values: 143.11
values: 142.98
values: 143.31
values: 143.28
values: 142.93
values: 143.18
values: 142.84
values: 143.13
values: 143.09
values: 142.8
values: 142.83
values: 142.88
values: 142.78
values: 142.96
values: 142.67
values: 143.07
values: 143.27
values: 144.51
values: 142.9
values: 143.03
values: 143.19
values: 143.29
values: 143.12
values: 143.08
values: 144.22
values: 142.77
values: 142.52
values: 142.79
values: 142.46
values: 142.44
values: 142.57
values: 142.37
values: 142.39
values: 142.65
values: 142.49
values: 142.5
values: 142.38
values: 142.73
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual mean temperature-tailored

t sid: lcRe8UyezlVixymjhu1
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 19.1071
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 19.7
values: 19.1
values: 18.6
values: 18.8
values: 18.5
values: 18.4
values: 18.3
values: 18.2
values: 18
values: 18.1
values: 18.9
values: 18.7
values: 19.4
values: 19
values: 19.5
values: 19.8
values: 20
values: 19.3
values: 19.2
values: 20.5
values: 19.6
values: 20.3
values: 20.7
values: 19.9
values: 16.8
values: 16
values: 17
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: annual precipitation-tailored

t sid: lcRXmngDjXALE1zPfXc
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.3606
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.36
values: 1.38
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: annual precipitation-tailored

t sid: lcR3Q7ugRgt2GXbASpl
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 5.9586
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 6.4
values: 5.4
values: 6.7
values: 5.2
values: 5.7
values: 5.1
values: 5.6
values: 5
values: 6
values: 5.3
values: 5.9
values: 7.1
values: 6.3
values: 6.1
values: 6.2
values: 6.8
values: 6.9
values: 7.4
values: 7.3
values: 8.6
values: 6.5
values: 6.6
values: 5.8
values: 7.2
values: 4.8
values: 5.5
values: 3.8
values: 3.1
values: 3.2
values: 1.6
values: 0.2
values: 1.7
values: 4.1
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual precipitation-tailored

t sid: lcRXno9hClyAg8b6ZED
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.8006
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.8
values: 1.82
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual precipitation-tailored

t sid: lcRMPkP0JPngepqKt5J
variable name: precipitation
units: mm/yr
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 1049.3057
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
QC certification: CH
q cnotes: Marked in original compilation as primary P timeseries; Pass age control and data resolution; pvalue <0.1
notes: null
values: 997.4
values: 973.8
values: 1115
values: 1061.3
values: 1068.6
values: 1132.6
values: 1089.7
values: 1172
values: 1099.3
values: 1152.2
values: 1173.9
values: 1121.9
values: 1124.7
values: 1084.3
values: 1165.2
values: 1101.4
values: 1112.7
values: 1171.2
values: 1099.2
values: 1106.3
values: 1080.4
values: 1071.8
values: 1118.8
values: 1128.7
values: 1119.6
values: 1066.9
values: 1076.2
values: 1099
values: 1060.4
values: 1083.4
values: 1090.8
values: 1139.2
values: 1104.7
values: 1050.4
values: 1084.5
values: 1086.7
values: 1014.6
values: 1072
values: 1078.9
values: 1093.2
values: 1158.4
values: 1117.7
values: 1032.2
values: 1105.9
values: 1121.1
values: 1124
values: 1128.2
values: 1093.8
values: 1120.8
values: 1018.3
values: 1035.9
values: 1006.3
values: 952.2
values: 938.5
values: 950.9
values: 958.3
values: 930.5
values: 889.9
values: 955.1
values: 914.5
values: 956
values: 934.6
values: 892.5
values: 872.4
values: 918.9

t sid: lcRUa5GobhtuETm0Hzj
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 115.7486
median res12k: 140
datum: abs
proxy: pollen
proxy detail: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 115.55
values: 115.43
values: 115.42
values: 115.39
values: 115.54
values: 115.51
values: 115.83
values: 115.71
values: 115.91
values: 115.73
values: 115.69
values: 115.66
values: 115.85
values: 115.84
values: 115.79
values: 116.01
values: 115.94
values: 115.74
values: 115.63
values: 115.8
values: 115.82
values: 115.76
values: 115.68
values: 115.75
values: 115.56
values: 115.67
values: 115.72
values: 115.77
values: 115.81
values: 116.16
values: 116.52
values: 116.02
values: 115.93
values: 116.19
values: 115.87
values: 115.61
values: 116.07
values: 115.57
values: 115.58
values: 116.06
values: 115.59
values: 115.6
values: 115.65
values: 115.95
values: 115.7
values: 115.52
values: 115.62
values: 115.92
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual precipitation-tailored

measurement table:
  table name: chron1measurement1
  lab ID:
    number: 1
    t sid: lc-chRpkCevrht3uOIVdRp
    variable name: labID
    units: unitless
    values: OS-72346
    values: OS-72350
    values: OS-72351
    values: OS-72352
    values: OS-72353
    values: OS-72354
  age type:
    number: 2
    t sid: lc-chRKsczWBfBoE4HOIGR
    variable name: age_type
    units: unitless
    values: Dates from prior information
    values: Carbon-14
  material dated:
    number: 3
    t sid: lc-chRAApc1PuSQk6U1gCB
    variable name: materialDated
    units: unitless
    values: bulk sediment
  depth:
    number: 4
    t sid: lc-chRHPLb4iORenAZVO1V
    variable name: depth
    units: cm
    values: 32.5
    values: 50.5
    values: 145.5
    values: 250.5
    values: 377.5
    values: 555.5
    values: 640.5
  thickness:
    number: 5
    t sid: lc-chRH8t2hHmgp2kAZufL
    variable name: thickness
    units: cm
    values: NA
    values: 1
  notes:
    number: 6
    t sid: lc-chRWcerz1SVMB9aE4bL
    variable name: notes
    units: unitless
  age14 c:
    number: 7
    t sid: lc-chRyHn10mLnU7NipOSS
    variable name: age14C
    units: yr BP 14C
    values: 130
    values: 1390
    values: 3710
    values: 4680
    values: 7670
    values: 9720
    values: 10200
  age:
    number: 8
    t sid: lc-chRXMdWySgClIxyd6B3
    variable name: age
    units: yr BP
    values: 130
    values: 1310
    values: 4050
    values: 5400
    values: 8470
    values: 11130
    values: 11870
  age uncertainty:
    number: 9
    t sid: lc-chRnMe9GGiSwOLYPL3u
    variable name: ageUncertainty
    units: yr BP
    summary statistic: 2 sigma
    values: 10
    values: 20
    values: 50
    values: 40
    values: 70
    values: 60
  age14 c uncertainty:
    number: 10
    t sid: lc-chRViRKvZf6Syi7y3y7
    variable name: age14CUncertainty
    units: yr BP 14C
    summary statistic: 1 sigma
    values: 10
    values: 30
    values: 40
    values: 50
  depth top:
    number: 11
    t sid: lc-chRa9Toh3Rf2mkwv57I
    variable name: depth_top
    units: cm
    values: NA
    values: 50
    values: 145
    values: 250
    values: 377
    values: 555
    values: 640
  depth bottom:
    number: 12
    t sid: lc-chRPkvXuCO1sJQBAhEt
    variable name: depth_bottom
    units: cm
    values: NA
    values: 51
    values: 146
    values: 251
    values: 378
    values: 556
    values: 641

version: 1.0.7
last version: 1.0.6
curator: nicholas
timestamp: 2023-08-10 23:03:57 UTC
changes:
  base metadata: originalDataUrl: 'https://doi.pangaea.de/10.1594/PANGAEA.930512' has been replaced by 'https://doi.org/10.1594/10.1594/PANGAEA.930512'

version: 1.0.6
last version: 1.0.5
curator: nicholas
timestamp: 2023-07-05 00:48:27 UTC
changes:
  paleo interpretation metadata: precipitation (lcRMPkP0JPngepqKt5J): interpretation1_variableDetail: 'precipitation@surface' has been replaced by 'amount@surface'

version: 1.0.5
last version: 1.0.4
curator: nicholas
timestamp: 2023-05-25 17:48:55 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  geographic metadata: geo_elevation: '' has been replaced by '253'

version: 1.0.4
last version: 1.0.3
curator: nicholas
timestamp: 2023-02-13 23:49:58 UTC
changes:
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRq2fIc4rEaL8HitjN): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRqfCsEy30NlQfew2H): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRRjuWEHVRbLBeeRyH): paleoData_notes: '' has been replaced by 'null'
  paleo interpretation metadata: uncertaintyHigh (lcRJR6bzPuJFl2ftWoi): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): interpretation1_scope: '' has been replaced by 'climate'

version: 1.0.3
last version: 1.0.2
curator: nicholas
timestamp: 2023-02-09 15:56:52 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  base metadata: archiveType: 'Lake' has been replaced by 'LakeSediment'
  paleo interpretation metadata: temperature (lcR3Q7ugRgt2GXbASpl): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcR4tKh8R0JknoMiYmG): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: uncertainty (lcR4tKh8R0JknoMiYmG): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcR5HjgKD1wkbXAbn2Y): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: uncertainty (lcR5HjgKD1wkbXAbn2Y): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcR5IymQT49lQwZoCf1): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: temperature (lcR64AHdbeC6hWUlwYg): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRe8UyezlVixymjhu1): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRe8UyezlVixymjhu1): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRfribY3hZ5nPLjOXo): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRhyCU1d7DO4spNHql): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRLhHuAeNYsXAxFBep): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcRMPkP0JPngepqKt5J): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
  paleo interpretation metadata: precipitation (lcRMPkP0JPngepqKt5J): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcRNEoFcKZwZ7McK9z9): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcROSAMWyIx6hXhQsRz): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRP188wuX5JZT0dU8X): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRP188wuX5JZT0dU8X): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: temperature (lcRplMkhCiVPIvwDFKV): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRplMkhCiVPIvwDFKV): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcRq2fIc4rEaL8HitjN): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: precipitation (lcRqfCsEy30NlQfew2H): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcRQkS2hE7FLTjylOUy): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRRfMoSqdPTDda1F8t): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: uncertainty (lcRRfMoSqdPTDda1F8t): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcRRjuWEHVRbLBeeRyH): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcRrWZYNBcSErwg5oGa): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRTMLOWthm9bcDABcd): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRUa5GobhtuETm0Hzj): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcRXmngDjXALE1zPfXc): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: uncertainty (lcRXmngDjXALE1zPfXc): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRXno9hClyAg8b6ZED): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: temperature (lcRYF2YGANynsAsu1hX): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRYF2YGANynsAsu1hX): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcR4tKh8R0JknoMiYmG): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcR4tKh8R0JknoMiYmG): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcR4tKh8R0JknoMiYmG): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcR5IymQT49lQwZoCf1): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcR5IymQT49lQwZoCf1): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcR5IymQT49lQwZoCf1): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: age (lcR6Zf0IQfOhT3ICqCB): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcR6Zf0IQfOhT3ICqCB): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: age (lcR6Zf0IQfOhT3ICqCB): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: depth (lcRD0fdGOjxSYe2H9Hp): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: depth (lcRD0fdGOjxSYe2H9Hp): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
  paleo column metadata: uncertainty (lcRfribY3hZ5nPLjOXo): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRfribY3hZ5nPLjOXo): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRfribY3hZ5nPLjOXo): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRfribY3hZ5nPLjOXo): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: age (lcRgQ9f7kUUFMjB6DXo): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcRgQ9f7kUUFMjB6DXo): paleoData_variableName: 'ageMedian' has been replaced by 'age'
  paleo column metadata: age (lcRgQ9f7kUUFMjB6DXo): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: age (lcRgQ9f7kUUFMjB6DXo): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertaintyHigh (lcRJR6bzPuJFl2ftWoi): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyHigh (lcRJR6bzPuJFl2ftWoi): paleoData_variableName: 'ageMax' has been replaced by 'uncertaintyHigh'
  paleo column metadata: uncertaintyHigh (lcRJR6bzPuJFl2ftWoi): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyHigh (lcRJR6bzPuJFl2ftWoi): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcRLhHuAeNYsXAxFBep): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRLhHuAeNYsXAxFBep): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRLhHuAeNYsXAxFBep): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): paleoData_variableName: 'ageMin' has been replaced by 'uncertaintyLow'
  paleo column metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): paleoData_inferredMaterial: '' has been replaced by 'age'
  paleo column metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyLow (lcRo2jHvsy5I2rJpCa2): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcROSAMWyIx6hXhQsRz): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcROSAMWyIx6hXhQsRz): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcROSAMWyIx6hXhQsRz): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcROSAMWyIx6hXhQsRz): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'

version: 1.0.2
last version: 1.0.1
curator: nicholas
timestamp: 2022-09-09 02:10:32 UTC
changes:
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_QCnotes: 'Marked in original compilation as primary P timeseries; Pass age control and data resolution' has been replaced by 'Marked in original compilation as primary P timeseries; Pass age control and data resolution; pvalue <0.1'
  paleo interpretation metadata: precipitation (lcRMPkP0JPngepqKt5J): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'

version: 1.0.1
last version: 1.0.0
curator: nicholas
timestamp: 2022-07-28 17:36:11 UTC
changes:
  base metadata: originalDataUrl: '' has been replaced by 'https://doi.pangaea.de/10.1594/PANGAEA.930512'
  publication metadata: pub1_year: '' has been replaced by '2018'
  publication metadata: pub1_author: '' has been replaced by 'Oswald, W.W., Foster, D.R., Shuman, B.N., Doughty, E.D., Faison, E.K., Hall, B.R., Hansen, B.C., Lindbladh, M., Marroquin, A. and Truebe, S.A.'
  publication metadata: pub1_doi: '' has been replaced by '10.1111/jbi.13407'
  publication metadata: pub1_journal: '' has been replaced by 'Journal of biogeography'
  publication metadata: pub1_title: '' has been replaced by 'Subregional variability in the response of New England vegetation to postglacial climate change.'
  publication metadata: pub2_doi: '' has been replaced by '10.5194/essd-2022-38'
  geographic metadata: geo_elevation: '253' has been replaced by ''
  geographic metadata: geo_gcmdLocation: '' has been replaced by 'North America>United States Of America>New Hampshire'
  paleo column metadata: temperature (lcR3Q7ugRgt2GXbASpl): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcR3Q7ugRgt2GXbASpl): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcR3Q7ugRgt2GXbASpl): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcR3Q7ugRgt2GXbASpl): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR4tKh8R0JknoMiYmG): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcR4tKh8R0JknoMiYmG): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR4tKh8R0JknoMiYmG): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcR4tKh8R0JknoMiYmG): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcR5HjgKD1wkbXAbn2Y): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR5IymQT49lQwZoCf1): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcR5IymQT49lQwZoCf1): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR5IymQT49lQwZoCf1): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcR5IymQT49lQwZoCf1): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcR64AHdbeC6hWUlwYg): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcR64AHdbeC6hWUlwYg): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcR64AHdbeC6hWUlwYg): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcR64AHdbeC6hWUlwYg): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRCyjWNZn4PM2ZBM0H): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRe8UyezlVixymjhu1): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRe8UyezlVixymjhu1): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRe8UyezlVixymjhu1): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRe8UyezlVixymjhu1): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRfribY3hZ5nPLjOXo): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcRfribY3hZ5nPLjOXo): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRfribY3hZ5nPLjOXo): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcRfribY3hZ5nPLjOXo): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRhyCU1d7DO4spNHql): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRhyCU1d7DO4spNHql): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRhyCU1d7DO4spNHql): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRhyCU1d7DO4spNHql): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRLhHuAeNYsXAxFBep): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcRLhHuAeNYsXAxFBep): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRLhHuAeNYsXAxFBep): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcRLhHuAeNYsXAxFBep): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_QCCertification: '' has been replaced by 'CH'
  paleo column metadata: precipitation (lcRMPkP0JPngepqKt5J): paleoData_QCnotes: '' has been replaced by 'Marked in original compilation as primary P timeseries; Pass age control and data resolution'
  paleo column metadata: precipitationUncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcRNEoFcKZwZ7McK9z9): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcROSAMWyIx6hXhQsRz): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcROSAMWyIx6hXhQsRz): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcROSAMWyIx6hXhQsRz): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcROSAMWyIx6hXhQsRz): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRP188wuX5JZT0dU8X): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRP188wuX5JZT0dU8X): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRP188wuX5JZT0dU8X): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRP188wuX5JZT0dU8X): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRplMkhCiVPIvwDFKV): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRplMkhCiVPIvwDFKV): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRplMkhCiVPIvwDFKV): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRplMkhCiVPIvwDFKV): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRq2fIc4rEaL8HitjN): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRq2fIc4rEaL8HitjN): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRq2fIc4rEaL8HitjN): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRq2fIc4rEaL8HitjN): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRqfCsEy30NlQfew2H): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRqfCsEy30NlQfew2H): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRqfCsEy30NlQfew2H): paleoData_proxyDetail: '' has been replaced by 'Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRqfCsEy30NlQfew2H): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRQkS2hE7FLTjylOUy): paleoData_datum: '' has been replaced by 'abs'

version: 1.0.0
curator: nicholas
timestamp: 2022-05-26 21:53:05 UTC
notes: Starting the changelog

Subregional variability in the response of New England vegetation to postglacial climate change.
author:
  name: Oswald, W.W., Foster, D.R., Shuman, B.N., Doughty, E.D., Faison, E.K., Hall, B.R., Hansen, B.C., Lindbladh, M., Marroquin, A. and Truebe, S.A.
citation: Oswald, W.W. et al. (2018)
year: 2018
doi: 10.1111/jbi.13407
journal: Journal of biogeography

doi: 10.5194/essd-2022-38

longitude: -71.1781
latitude: 43.2917
elevation: 253
description: Tsuga candensis, Fagus grandifolia, Acer saccharum, Pinus strobus, and Betula species are common in the northern, inland, and higher-elevation parts of New England. Quercus, Carya, and Castanea dentata dominate in the warmer southern part of the region. Acer rubrum is common across New England. Pinus rigida is prevalent on sites with well-drained sandy soils.
site name: Little Willey Pond
continent: Eastern North America
gcmd location: North America>United States Of America>New Hampshire