paleo data:
  measurement table:
    table name: paleo1measurement1
    uncertainty low:
      t sid: lcRTvaqyqYD2keeMxuT
      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: 260
      mean value12k: 6307.75
      values: 20
      values: 250
      values: 500
      values: 770
      values: 1230
      values: 1560
      values: 1980
      values: 2180
      values: 2330
      values: 2620
      values: 3260
      values: 3930
      values: 4500
      values: 4960
      values: 5090
      values: 5160
      values: 5720
      values: 6020
      values: 6430
      values: 6740
      values: 7320
      values: 7450
      values: 7500
      values: 7630
      values: 7790
      values: 8060
      values: 8890
      values: 9320
      values: 9590
      values: 9680
      values: 9750
      values: 9880
      values: 9990
      values: 10160
      values: 10260
      values: 10350
      values: 10450
      values: 10620
      values: 11100
      values: 11270
      values: 11440
      values: 11880
      values: 12670
      values: 13620
      values: 14080
      values: 14450
      interpretation:
        scope: climate
    uncertainty high:
      t sid: lcRjxJhwVhkSW4BSJNJ
      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: 260
      mean value12k: 6809.25
      values: 780
      values: 1000
      values: 1260
      values: 1470
      values: 1660
      values: 2080
      values: 2360
      values: 2600
      values: 2820
      values: 3120
      values: 3690
      values: 4610
      values: 4900
      values: 5270
      values: 5390
      values: 5820
      values: 6340
      values: 6450
      values: 6660
      values: 7050
      values: 7480
      values: 7680
      values: 7770
      values: 8110
      values: 8970
      values: 9410
      values: 9530
      values: 9670
      values: 10000
      values: 10100
      values: 10190
      values: 10230
      values: 10300
      values: 10500
      values: 10600
      values: 10780
      values: 10960
      values: 11080
      values: 11610
      values: 12070
      values: 14120
      values: 14830
      values: 15460
      values: 15920
      values: 16300
      values: 17310
      interpretation:
        scope: climate
    age:
      t sid: lcR6exlrp7sEemfnpkv
      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: 310
      values: 590
      values: 860
      values: 1170
      values: 1470
      values: 1770
      values: 2150
      values: 2280
      values: 2480
      values: 2920
      values: 3480
      values: 4220
      values: 4660
      values: 5120
      values: 5260
      values: 5420
      values: 6080
      values: 6270
      values: 6530
      values: 6900
      values: 7400
      values: 7540
      values: 7590
      values: 7810
      values: 8280
      values: 8950
      values: 9300
      values: 9550
      values: 9800
      values: 9910
      values: 10020
      values: 10130
      values: 10220
      values: 10350
      values: 10430
      values: 10530
      values: 10690
      values: 10830
      values: 11220
      values: 11530
      values: 12350
      values: 13320
      values: 14310
      values: 15230
      values: 15930
      values: 16440
    age-1:
      t sid: lcRRXERgvt39nchMxxK
      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: 320
      values: 600
      values: 870
      values: 1150
      values: 1460
      values: 1780
      values: 2160
      values: 2340
      values: 2520
      values: 2910
      values: 3480
      values: 4240
      values: 4670
      values: 5120
      values: 5250
      values: 5440
      values: 6060
      values: 6260
      values: 6540
      values: 6910
      values: 7400
      values: 7550
      values: 7600
      values: 7830
      values: 8320
      values: 8890
      values: 9280
      values: 9550
      values: 9800
      values: 9910
      values: 10010
      values: 10110
      values: 10200
      values: 10350
      values: 10420
      values: 10540
      values: 10690
      values: 10840
      values: 11260
      values: 11570
      values: 12460
      values: 13340
      values: 14240
      values: 15130
      values: 15810
      values: 16370
archive type: LakeSediment
data set name: DeepTauntonPond.Oswald.2018
dataset id: LC5d10d37c97adb1b5563932315656bda4
created by: github.com/nickmckay/LegacyClimate2LiPD
original data source: Neotoma
legacy climate site id: 23609
legacy climate dataset id: 40844
ages per kyr: NA
max year: 16440
min year: 310
original data url: https://doi.org/10.1594/10.1594/PANGAEA.930512
lipdverse link: https://lipdverse.org/data/LC5d10d37c97adb1b5563932315656bda4/1_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.

t sid: lcRvT83MUETeRt0vsLT
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: 32
values: 64
values: 96
values: 128
values: 160
values: 192
values: 224
values: 256
values: 288
values: 320
values: 384
values: 448
values: 480
values: 544
values: 560
values: 576
values: 624
values: 640
values: 656
values: 672
values: 688
values: 704
values: 720
values: 736
values: 752
values: 768
values: 784
values: 800
values: 832
values: 848
values: 864
values: 880
values: 896
values: 928
values: 944
values: 960
values: 976
values: 992
values: 1028
values: 1040
values: 1056
values: 1072
values: 1088
values: 1104
values: 1120
values: 1152

t sid: lcRtIxog1fpHMZyseqS
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 20.3875
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 20.6
values: 21
values: 20.5
values: 20.9
values: 21.4
values: 20.7
values: 20.3
values: 21.3
values: 22
values: 20.2
values: 21.2
values: 20.1
values: 20.4
values: 20
values: 19.6
values: 19.8
values: 19.3
values: 19.1
values: 19.9
values: 18.9
values: 18
values: 15.2
values: 17
values: 17.9
values: 17.1
values: 16.1
values: 14.8
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRNzjS1Rp3vbLFi6hq
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.4425
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.44
values: 1.45
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRbgC0mgaTnqmKSqBb
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 20.54
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 20.8
values: 20.5
values: 20.9
values: 21.2
values: 20.3
values: 21.6
values: 20.6
values: 21.7
values: 20.7
values: 21
values: 21.1
values: 21.3
values: 19.5
values: 19.1
values: 19.4
values: 18.5
values: 19.6
values: 20.4
values: 19.3
values: 18
values: 17.6
values: 16.4
values: 18.3
values: 18.2
values: 15.9
values: 14.2
values: 13.5
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcRP9QGvSJc4p4VAvZs
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.1273
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 0.99
values: 1.18
values: 1.3
values: 1.28
values: 1.27
values: 1.29
values: 1.22
values: 1.23
values: 1.2
values: 1.1
values: 1.14
values: 1.11
values: 1.07
values: 1.12
values: 1.05
values: 1.13
values: 1.06
values: 1.15
values: 1
values: 1.02
values: 1.4
values: 1.39
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcRcLMZkQDL3u0aHob5
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 6.825
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 7.2
values: 7.8
values: 6.8
values: 8
values: 7.1
values: 9
values: 7.7
values: 8.3
values: 7.5
values: 7.3
values: 7.6
values: 8.6
values: 10
values: 8.9
values: 6.5
values: 8.7
values: 6.6
values: 7
values: 6.7
values: 6.3
values: 6.9
values: 6
values: 5.9
values: 6.1
values: 5.2
values: 5.7
values: 4.8
values: 4.6
values: 5.4
values: 4
values: 3.2
values: -0.8
values: 1.5
values: 2.9
values: 2.1
values: 0.1
values: -2.3
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRUfuPtr1Fu2SA7MPZ
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 2.0793
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 2.08
values: 2.09
values: 2.07
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRrrN4JCYa4TLa61qW
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 7.62
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 8.3
values: 8
values: 9.3
values: 9.2
values: 9.1
values: 8.6
values: 8.4
values: 8.9
values: 8.2
values: 9
values: 8.5
values: 7.8
values: 7.9
values: 7.6
values: 8.1
values: 5.7
values: 5
values: 5.6
values: 5.5
values: 4.6
values: 5.4
values: 6.9
values: 5.1
values: 3.8
values: 2.4
values: -0.3
values: 0.4
values: 0.5
values: -0.5
values: -2.8
values: -2.4
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRKH0GYQovsPPeuDK9
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.511
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.46
values: 1.41
values: 1.56
values: 1.53
values: 1.52
values: 1.54
values: 1.55
values: 1.45
values: 1.49
values: 1.43
values: 1.38
values: 1.4
values: 1.47
values: 1.42
values: 1.37
values: 1.5
values: 1.51
values: 1.65
values: 1.81
values: 1.58
values: 1.77
values: 1.59
values: 1.33
values: 2.03
values: 1.35
values: 1.34
values: 1.36
values: 1.32
values: 2.59
values: 1.31
values: 1.85
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRW2jFEVcD4fndLl66
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 985.7275
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 1014.2
values: 1020.8
values: 996.1
values: 1094.8
values: 967.6
values: 1026.5
values: 1145.3
values: 1085.8
values: 1054.6
values: 1077.8
values: 1051.8
values: 1050.5
values: 1052.8
values: 1082
values: 1002.6
values: 1093.8
values: 1187.1
values: 1120
values: 970.1
values: 1113.4
values: 1048.4
values: 1003.3
values: 896.7
values: 976.7
values: 922.1
values: 963.6
values: 927.2
values: 947
values: 890.6
values: 922
values: 851.1
values: 868.1
values: 904
values: 870.8
values: 846.6
values: 910.5
values: 803.4
values: 874.6
values: 854.5
values: 940.3
values: 878.6
values: 872.8
values: 929
values: 1016.2
values: 790.5
values: 525.9
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRC6qYpgcDVta6jJr5
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 169.0673
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 168.91
values: 168.99
values: 169.05
values: 169.09
values: 169.01
values: 169.15
values: 169.11
values: 169.21
values: 169.17
values: 169.16
values: 169
values: 169.08
values: 169.02
values: 169.46
values: 169.41
values: 169.28
values: 169.04
values: 168.92
values: 168.8
values: 168.93
values: 168.78
values: 168.98
values: 169.12
values: 169.29
values: 169.19
values: 168.94
values: 169.23
values: 168.84
values: 168.83
values: 168.87
values: 170.02
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRyelthCDI1iH3kgw2
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 994.715
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 989.8
values: 1086.6
values: 1189.2
values: 1143.1
values: 1198.6
values: 1168.8
values: 1162.4
values: 1181.1
values: 1178.7
values: 1203.7
values: 1225.7
values: 1054.5
values: 1156.8
values: 1114.9
values: 1093.2
values: 1048.9
values: 1035.2
values: 1056.1
values: 1023.2
values: 1061.6
values: 1081.6
values: 1040.8
values: 934.8
values: 949.3
values: 991.8
values: 854.7
values: 903.7
values: 890.2
values: 910.4
values: 899
values: 774
values: 784
values: 778.5
values: 771.7
values: 803.7
values: 777.1
values: 817.9
values: 809.2
values: 833.8
values: 810.3
values: 830.3
values: 762.3
values: 741.9
values: 975.7
values: 821.1
values: 864.4
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRlQnNoEOV05DO7qh1
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 145.069
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 134.57
values: 171.51
values: 171.13
values: 168.57
values: 171.19
values: 160.33
values: 164.11
values: 170.89
values: 170.79
values: 176.57
values: 170.61
values: 149.99
values: 170.81
values: 154.34
values: 132.86
values: 134.36
values: 168.3
values: 139.44
values: 135.5
values: 170.65
values: 135.74
values: 141.2
values: 132.4
values: 141.3
values: 148.7
values: 131.58
values: 130.84
values: 134.95
values: 129.92
values: 121.39
values: 131.71
values: 121.37
values: 121.72
values: 122.39
values: 121.53
values: 140.46
values: 128.47
values: 121.88
values: 125.83
values: 126.15
values: 126.02
values: 175.63
values: 171.2
values: 145.47
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRcW8ytR6pozkNA2Fp
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 20.48
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 20.9
values: 21
values: 20.7
values: 20.8
values: 21.1
values: 20.6
values: 20.5
values: 21.3
values: 21.6
values: 21.2
values: 20.4
values: 20.3
values: 20
values: 19.8
values: 19.9
values: 19.6
values: 19.1
values: 20.1
values: 19.3
values: 18.4
values: 16.2
values: 17.6
values: 18.2
values: 17.3
values: 17
values: 16
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: lcR51VNtuj6Sqli6sXf
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.0568
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.05
values: 1.06
values: 1.07
values: 1.09
values: 1.08
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: lcRlIluL6mZkznNr3lA
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 993.9025
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 1060
values: 1050.5
values: 1036.3
values: 1123.5
values: 993
values: 1055.2
values: 1150.6
values: 1106.5
values: 1096.3
values: 1087.2
values: 1086.9
values: 1101.6
values: 1127.9
values: 1032.6
values: 1154.7
values: 1221.5
values: 1178.3
values: 1030
values: 1104.4
values: 1092.7
values: 1031.7
values: 954.8
values: 994.2
values: 933.2
values: 966.7
values: 935.8
values: 950
values: 879.1
values: 938.1
values: 792.2
values: 800.2
values: 865.9
values: 837.9
values: 776.9
values: 847.3
values: 725.3
values: 806.8
values: 822.1
values: 901.7
values: 870.3
values: 816.9
values: 858.7
values: 963
values: 802.3
values: 536.6
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: lcRsQ0jZLrrxLi4GX0b
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 158.0475
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 157.81
values: 157.97
values: 158
values: 157.92
values: 158.15
values: 158.23
values: 158.1
values: 158.09
values: 158.24
values: 158.13
values: 157.93
values: 158.06
values: 158.35
values: 158.57
values: 157.87
values: 158.07
values: 158.05
values: 157.75
values: 157.99
values: 157.8
values: 157.88
values: 157.71
values: 158.11
values: 158.21
values: 158.12
values: 157.91
values: 158.39
values: 157.96
values: 158.02
values: 157.89
values: 158.33
values: 158.25
values: 158.34
values: 158.41
values: 160.79
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: lcRH7OrttyiTGz6f0ks
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 7.12
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 8.1
values: 8.2
values: 7.6
values: 8.6
values: 7.5
values: 8.4
values: 9.1
values: 8.5
values: 7.7
values: 8.8
values: 9.8
values: 10.5
values: 10
values: 7.2
values: 6.6
values: 7.1
values: 6.3
values: 5.9
values: 5.1
values: 4.5
values: 5.4
values: 4.6
values: 3.7
values: 4.3
values: 4.8
values: 3.8
values: 3
values: -0.2
values: 1.2
values: 2.1
values: 1.6
values: 0.6
values: -1.9
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: lcRZjcGeNbLakhaTtOH
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.5003
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.5
values: 1.51
values: 1.52
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: lcR6Bwz2j54tSfbme5P
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 997.9025
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
notes: null
values: 1069.7
values: 1057.1
values: 1041.6
values: 1131
values: 998.2
values: 1058
values: 1151.3
values: 1111.3
values: 1102.8
values: 1118.2
values: 1095.5
values: 1092.1
values: 1108
values: 1139
values: 1036.7
values: 1161.6
values: 1221.1
values: 1178.5
values: 1032.6
values: 1104
values: 1094.2
values: 1030.7
values: 961.5
values: 995.8
values: 934.4
values: 967
values: 937.2
values: 954.3
values: 878
values: 942.1
values: 797.3
values: 806.3
values: 871.4
values: 840.9
values: 777.4
values: 853.8
values: 726.8
values: 810.8
values: 831.3
values: 896.6
values: 854
values: 815.7
values: 854.5
values: 951.3
values: 790.8
values: 541.4
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: lcRivo4BSlFTomNpkkT
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 152.7405
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 151.84
values: 151.94
values: 152.11
values: 152.41
values: 152.35
values: 153.21
values: 153.11
values: 152.68
values: 152.73
values: 152.66
values: 152.42
values: 152.51
values: 152.47
values: 152.27
values: 153.12
values: 153.85
values: 153.28
values: 152.39
values: 153.05
values: 152.6
values: 153.46
values: 152.12
values: 153.1
values: 152.26
values: 152.53
values: 151.91
values: 152.7
values: 153.74
values: 153.75
values: 153.13
values: 152.97
values: 153.43
values: 154.33
values: 152.75
values: 152.52
values: 152.02
values: 152.05
values: 152.1
values: 152.07
values: 152.24
values: 153.9
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: lcRiiYTSjw2vZkUKQmM
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 20.6725
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 21
values: 21.3
values: 20.9
values: 21.2
values: 21.7
values: 21.1
values: 20.4
values: 21.8
values: 22.4
values: 21.9
values: 20.6
values: 20.5
values: 20.8
values: 20.2
values: 19.8
values: 20
values: 19.5
values: 19.1
values: 20.1
values: 18.2
values: 15.5
values: 17.3
values: 17.4
values: 16.3
values: 15
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: lcRMp2pdDMrP6d2bDpl
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.3802
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.38
values: 1.39
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: lcRORwKTmWw9A2LewfG
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 7.6275
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
values: 8.2
values: 8.5
values: 7.9
values: 9
values: 8.8
values: 9.9
values: 8.6
values: 8.7
values: 7.6
values: 9.3
values: 8.4
values: 8.3
values: 11.1
values: 10.1
values: 9.1
values: 7.8
values: 8.1
values: 7.7
values: 7.5
values: 7.1
values: 6.7
values: 6.8
values: 6.9
values: 6.3
values: 5.7
values: 6.2
values: 5.4
values: 4.9
values: 7
values: 5.8
values: 6.1
values: 4.5
values: 3.7
values: -0.2
values: 1.9
values: 3.1
values: 2.4
values: 0.5
values: -2.2
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: lcRoXElriMnKQ39tKkZ
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.856
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.86
values: 1.85
values: 1.87
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: lcRgG0nqmKpMbG6TnGY
variable name: precipitation
units: mm/yr
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 1017.7925
median res12k: 260
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 rigada 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: 1051.6
values: 1051.7
values: 1043.8
values: 1105.8
values: 1017.1
values: 1074.4
values: 1150
values: 1103.9
values: 1103
values: 1102.1
values: 1050.9
values: 1083.1
values: 1074.9
values: 1100.7
values: 1039.3
values: 1131.2
values: 1194.9
values: 1152.8
values: 1024.6
values: 1084.3
values: 1053.9
values: 963.8
values: 1005.4
values: 957.9
values: 999.6
values: 963
values: 955.9
values: 941.4
values: 965.6
values: 897.5
values: 906.9
values: 941
values: 914.5
values: 885.2
values: 930.6
values: 866.6
values: 885.4
values: 886.6
values: 950.1
values: 881
values: 868.2
values: 902.2
values: 983.7
values: 812.5
values: 522.4
interpretation:
  scope: climate
  variable: precipitation
  variable detail: amount@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: annual precipitation-tailored
in compilation beta:
  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
in compilation beta:
  compilation name: HoloceneAbruptChange
  compilation version: 0_11_0

t sid: lcR94qUaJIxvy226IrG
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 121.8178
median res12k: 260
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 rigada is prevalent on sites with well-drained sandy soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 121.73
values: 121.77
values: 121.72
values: 121.75
values: 121.82
values: 121.83
values: 121.89
values: 121.91
values: 121.93
values: 121.9
values: 121.74
values: 121.96
values: 122.17
values: 121.94
values: 121.8
values: 121.79
values: 121.78
values: 121.69
values: 121.68
values: 121.59
values: 121.7
values: 121.61
values: 121.97
values: 121.81
values: 122.03
values: 122.08
values: 121.64
values: 121.67
values: 121.98
values: 121.71
values: 122.67
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-chRKZCikjtsn5u291qh
    variable name: labID
    units: unitless
    values: OS-108284
    values: OS-108285
    values: OS-108286
    values: OS-108287
    values: OS-108315
    values: OS-108316
    values: OS-108317
    values: OS-108318
    values: OS-108319
    values: OS-108320
    values: OS-108321
    values: OS-108322
    values: OS-108323
    values: OS-108324
    values: OS-108482
    values: OS-108483
    values: OS-108544
  age type:
    number: 2
    t sid: lc-chRmHehl8tt0Sed0WC9
    variable name: age_type
    units: unitless
    values: Dates from prior information
    values: Carbon-14
  material dated:
    number: 3
    t sid: lc-chR2ciBlmBcKJYYAsml
    variable name: materialDated
    units: unitless
    values: sediment
  depth:
    number: 4
    t sid: lc-chRoz32MCr6tUOKyRoq
    variable name: depth
    units: cm
    values: 32
    values: 64.5
    values: 172.5
    values: 232.5
    values: 274.5
    values: 348.5
    values: 420.5
    values: 474.5
    values: 554.5
    values: 650.5
    values: 676.5
    values: 692.5
    values: 730.5
    values: 800.5
    values: 892.5
    values: 946.5
    values: 1004.5
    values: 1030.5
    values: 1122.5
  thickness:
    number: 5
    t sid: lc-chRuT42PCWpHxXEtX4a
    variable name: thickness
    units: cm
    values: NA
    values: 1
  notes:
    number: 6
    t sid: lc-chR4rrzQIaHVU660YAB
    variable name: notes
    units: unitless
  age14 c:
    number: 7
    t sid: lc-chRunwW24B05KuwiILn
    variable name: age14C
    units: yr BP 14C
    values: 200
    values: 310
    values: 1660
    values: 2360
    values: 2280
    values: 3020
    values: 3490
    values: 4110
    values: 4510
    values: 5640
    values: 6140
    values: 6690
    values: 6720
    values: 8620
    values: 9050
    values: 9150
    values: 9640
    values: 9800
    values: 13400
  age:
    number: 8
    t sid: lc-chRYGz8z6Nb8aiBw3v3
    variable name: age
    units: yr BP
    values: 200
    values: 310
    values: 1550
    values: 2380
    values: 2280
    values: 3220
    values: 3760
    values: 4650
    values: 5160
    values: 6420
    values: 7050
    values: 7550
    values: 7580
    values: 9590
    values: 10210
    values: 10330
    values: 10990
    values: 11220
    values: 16130
  age uncertainty:
    number: 9
    t sid: lc-chRvEgb4GcUpftd4LDm
    variable name: ageUncertainty
    units: yr BP
    summary statistic: 2 sigma
    values: 50
    values: 0
    values: 30
    values: 60
    values: 40
    values: 80
    values: 70
    values: 20
    values: 110
    values: 100
  age14 c uncertainty:
    number: 10
    t sid: lc-chRclOKZRpOtuEq6Sn3
    variable name: age14CUncertainty
    units: yr BP 14C
    summary statistic: 1 sigma
    values: 50
    values: 0
    values: 30
    values: 40
    values: 70
  depth top:
    number: 11
    t sid: lc-chRKCfFP3QAOvtPf9u4
    variable name: depth_top
    units: cm
    values: NA
    values: 172
    values: 232
    values: 274
    values: 348
    values: 420
    values: 474
    values: 554
    values: 650
    values: 676
    values: 692
    values: 730
    values: 800
    values: 892
    values: 946
    values: 1004
    values: 1030
    values: 1122
  depth bottom:
    number: 12
    t sid: lc-chRMoG6YZZdd3lLYjeL
    variable name: depth_bottom
    units: cm
    values: NA
    values: 173
    values: 233
    values: 275
    values: 349
    values: 421
    values: 475
    values: 555
    values: 651
    values: 677
    values: 693
    values: 731
    values: 801
    values: 893
    values: 947
    values: 1005
    values: 1031
    values: 1123

version: 1.0.7
last version: 1.0.6
curator: nicholas
timestamp: 2023-08-10 22:47:35 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 00:37:39 UTC
changes:
  paleo interpretation metadata: precipitation (lcRgG0nqmKpMbG6TnGY): 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 17:41:13 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  geographic metadata: geo_elevation: '' has been replaced by '4'

version: 1.0.4
last version: 1.0.3
curator: nicholas
timestamp: 2023-02-13 23:40:45 UTC
changes:
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRW2jFEVcD4fndLl66): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRyelthCDI1iH3kgw2): paleoData_notes: '' has been replaced by 'null'
  paleo interpretation metadata: uncertaintyHigh (lcRjxJhwVhkSW4BSJNJ): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): interpretation1_scope: '' has been replaced by 'climate'

version: 1.0.3
last version: 1.0.2
curator: nicholas
timestamp: 2023-02-09 15:37:48 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  base metadata: archiveType: 'Lake' has been replaced by 'LakeSediment'
  paleo column metadata: uncertainty (lcR51VNtuj6Sqli6sXf): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcR51VNtuj6Sqli6sXf): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcR51VNtuj6Sqli6sXf): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: age (lcR6exlrp7sEemfnpkv): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcR6exlrp7sEemfnpkv): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: age (lcR6exlrp7sEemfnpkv): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcR94qUaJIxvy226IrG): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcR94qUaJIxvy226IrG): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcR94qUaJIxvy226IrG): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcR94qUaJIxvy226IrG): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRC6qYpgcDVta6jJr5): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRC6qYpgcDVta6jJr5): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRC6qYpgcDVta6jJr5): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRC6qYpgcDVta6jJr5): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRivo4BSlFTomNpkkT): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRivo4BSlFTomNpkkT): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRivo4BSlFTomNpkkT): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRivo4BSlFTomNpkkT): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertaintyHigh (lcRjxJhwVhkSW4BSJNJ): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyHigh (lcRjxJhwVhkSW4BSJNJ): paleoData_variableName: 'ageMax' has been replaced by 'uncertaintyHigh'
  paleo column metadata: uncertaintyHigh (lcRjxJhwVhkSW4BSJNJ): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyHigh (lcRjxJhwVhkSW4BSJNJ): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcRKH0GYQovsPPeuDK9): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRKH0GYQovsPPeuDK9): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRKH0GYQovsPPeuDK9): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRlQnNoEOV05DO7qh1): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRlQnNoEOV05DO7qh1): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRlQnNoEOV05DO7qh1): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRlQnNoEOV05DO7qh1): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRoXElriMnKQ39tKkZ): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRoXElriMnKQ39tKkZ): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRoXElriMnKQ39tKkZ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRP9QGvSJc4p4VAvZs): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRP9QGvSJc4p4VAvZs): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRP9QGvSJc4p4VAvZs): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: age (lcRRXERgvt39nchMxxK): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcRRXERgvt39nchMxxK): paleoData_variableName: 'ageMedian' has been replaced by 'age'
  paleo column metadata: age (lcRRXERgvt39nchMxxK): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: age (lcRRXERgvt39nchMxxK): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcRsQ0jZLrrxLi4GX0b): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRsQ0jZLrrxLi4GX0b): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRsQ0jZLrrxLi4GX0b): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRsQ0jZLrrxLi4GX0b): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): paleoData_variableName: 'ageMin' has been replaced by 'uncertaintyLow'
  paleo column metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): paleoData_inferredMaterial: '' has been replaced by 'age'
  paleo column metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyLow (lcRTvaqyqYD2keeMxuT): 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 (lcRUfuPtr1Fu2SA7MPZ): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRUfuPtr1Fu2SA7MPZ): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRUfuPtr1Fu2SA7MPZ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: depth (lcRvT83MUETeRt0vsLT): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: depth (lcRvT83MUETeRt0vsLT): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
  paleo column metadata: precipitation (lcRW2jFEVcD4fndLl66): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: precipitation (lcRyelthCDI1iH3kgw2): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRZjcGeNbLakhaTtOH): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRZjcGeNbLakhaTtOH): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRZjcGeNbLakhaTtOH): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo interpretation metadata: uncertainty (lcR51VNtuj6Sqli6sXf): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: uncertainty (lcR51VNtuj6Sqli6sXf): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcR6Bwz2j54tSfbme5P): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: uncertainty (lcR94qUaJIxvy226IrG): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRbgC0mgaTnqmKSqBb): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRbgC0mgaTnqmKSqBb): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: uncertainty (lcRC6qYpgcDVta6jJr5): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo interpretation metadata: temperature (lcRcLMZkQDL3u0aHob5): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: temperature (lcRcW8ytR6pozkNA2Fp): interpretation1_seasonality: 'July' has been replaced by 'Jul'
  paleo interpretation metadata: temperature (lcRcW8ytR6pozkNA2Fp): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: precipitation (lcRgG0nqmKpMbG6TnGY): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
  paleo interpretation metadata: precipitation (lcRgG0nqmKpMbG6TnGY): interpretation1_variable: 'P' has been replaced by 'precipitation'

version: 1.0.2
last version: 1.0.1
curator: nicholas
timestamp: 2022-09-09 02:04:55 UTC
changes:
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): 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 (lcRgG0nqmKpMbG6TnGY): 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 17:29:59 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: '4' has been replaced by ''
  geographic metadata: geo_gcmdLocation: '' has been replaced by 'North America>United States Of America>Massachusetts'
  paleo column metadata: temperatureUncertainty (lcR51VNtuj6Sqli6sXf): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcR51VNtuj6Sqli6sXf): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcR51VNtuj6Sqli6sXf): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcR51VNtuj6Sqli6sXf): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcR6Bwz2j54tSfbme5P): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcR94qUaJIxvy226IrG): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcR94qUaJIxvy226IrG): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcR94qUaJIxvy226IrG): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcR94qUaJIxvy226IrG): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRbgC0mgaTnqmKSqBb): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRbgC0mgaTnqmKSqBb): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRbgC0mgaTnqmKSqBb): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRbgC0mgaTnqmKSqBb): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRC6qYpgcDVta6jJr5): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcRC6qYpgcDVta6jJr5): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRC6qYpgcDVta6jJr5): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcRC6qYpgcDVta6jJr5): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRcLMZkQDL3u0aHob5): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRcLMZkQDL3u0aHob5): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRcLMZkQDL3u0aHob5): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRcLMZkQDL3u0aHob5): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRcW8ytR6pozkNA2Fp): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRcW8ytR6pozkNA2Fp): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRcW8ytR6pozkNA2Fp): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRcW8ytR6pozkNA2Fp): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_QCCertification: '' has been replaced by 'CH'
  paleo column metadata: precipitation (lcRgG0nqmKpMbG6TnGY): paleoData_QCnotes: '' has been replaced by 'Marked in original compilation as primary P timeseries; Pass age control and data resolution'
  paleo column metadata: temperature (lcRH7OrttyiTGz6f0ks): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRH7OrttyiTGz6f0ks): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRH7OrttyiTGz6f0ks): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRH7OrttyiTGz6f0ks): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRiiYTSjw2vZkUKQmM): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRiiYTSjw2vZkUKQmM): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRiiYTSjw2vZkUKQmM): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRiiYTSjw2vZkUKQmM): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRivo4BSlFTomNpkkT): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcRivo4BSlFTomNpkkT): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRivo4BSlFTomNpkkT): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcRivo4BSlFTomNpkkT): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRKH0GYQovsPPeuDK9): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcRKH0GYQovsPPeuDK9): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRKH0GYQovsPPeuDK9): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcRKH0GYQovsPPeuDK9): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitation (lcRlIluL6mZkznNr3lA): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRlQnNoEOV05DO7qh1): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: precipitationUncertainty (lcRlQnNoEOV05DO7qh1): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: precipitationUncertainty (lcRlQnNoEOV05DO7qh1): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: precipitationUncertainty (lcRlQnNoEOV05DO7qh1): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRMp2pdDMrP6d2bDpl): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcRMp2pdDMrP6d2bDpl): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperatureUncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRNzjS1Rp3vbLFi6hq): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperatureUncertainty (lcRNzjS1Rp3vbLFi6hq): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRORwKTmWw9A2LewfG): paleoData_datum: '' has been replaced by 'abs'
  paleo column metadata: temperature (lcRORwKTmWw9A2LewfG): paleoData_proxy: '' has been replaced by 'pollen'
  paleo column metadata: temperature (lcRORwKTmWw9A2LewfG): 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 rigada is prevalent on sites with well-drained sandy soils.'
  paleo column metadata: temperature (lcRORwKTmWw9A2LewfG): paleoData_proxyGeneral: '' has been replaced by 'pollen'
  paleo column metadata: temperatureUncertainty (lcRoXElriMnKQ39tKkZ): paleoData_datum: '' has been replaced by 'abs'

version: 1.0.0
curator: nicholas
timestamp: 2022-05-26 21:53:04 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: -71.012
latitude: 41.8822
elevation: 4
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 rigada is prevalent on sites with well-drained sandy soils.
site name: Deep-Taunton Pond
continent: Eastern North America
gcmd location: North America>United States Of America>Massachusetts