paleo data:
  measurement table:
    table name: paleo1measurement1
    uncertainty low:
      t sid: lcRcfqHRUf3HJKYVf6D
      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: 60
      mean value12k: 3591.1111
      values: -60
      values: -50
      values: -40
      values: -30
      values: -20
      values: -10
      values: 0
      values: 10
      values: 20
      values: 30
      values: 50
      values: 60
      values: 80
      values: 90
      values: 110
      values: 120
      values: 130
      values: 160
      values: 180
      values: 210
      values: 230
      values: 260
      values: 280
      values: 300
      values: 330
      values: 360
      values: 380
      values: 400
      values: 420
      values: 450
      values: 470
      values: 650
      values: 690
      values: 1140
      values: 1220
      values: 1360
      values: 1400
      values: 1520
      values: 1590
      values: 1710
      values: 1820
      values: 1930
      values: 2000
      values: 2050
      values: 2090
      values: 2150
      values: 2250
      values: 2500
      values: 2930
      values: 3420
      values: 3530
      values: 3590
      values: 3690
      values: 3810
      values: 3940
      values: 3960
      values: 4080
      values: 4240
      values: 4320
      values: 4430
      values: 4470
      values: 4520
      values: 4570
      values: 4620
      values: 4650
      values: 4670
      values: 4730
      values: 4820
    uncertainty high:
      t sid: lcRBe6MA38yyyZF7q3S
      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: 60
      mean value12k: 4195.4762
      values: -60
      values: -50
      values: -40
      values: -30
      values: -20
      values: -10
      values: 0
      values: 10
      values: 20
      values: 60
      values: 140
      values: 210
      values: 290
      values: 340
      values: 360
      values: 390
      values: 430
      values: 470
      values: 500
      values: 530
      values: 570
      values: 610
      values: 640
      values: 670
      values: 740
      values: 770
      values: 800
      values: 820
      values: 860
      values: 880
      values: 900
      values: 930
      values: 960
      values: 990
      values: 1000
      values: 1010
      values: 1080
      values: 1090
      values: 1390
      values: 2060
      values: 2310
      values: 2360
      values: 2580
      values: 2710
      values: 2850
      values: 2970
      values: 3120
      values: 3150
      values: 3190
      values: 3250
      values: 3290
      values: 3320
      values: 3450
      values: 3590
      values: 3700
      values: 4010
      values: 4140
      values: 4290
      values: 4450
      values: 4580
      values: 4610
      values: 4700
      values: 4810
      values: 4870
      values: 4910
      values: 4940
      values: 4970
      values: 5000
      values: 5030
    age:
      t sid: lcR9LOURf4cVBkltT1v
      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: -60
      values: -50
      values: -40
      values: -30
      values: -20
      values: -10
      values: 0
      values: 10
      values: 30
      values: 50
      values: 80
      values: 100
      values: 120
      values: 150
      values: 180
      values: 200
      values: 230
      values: 260
      values: 290
      values: 320
      values: 350
      values: 380
      values: 420
      values: 480
      values: 500
      values: 530
      values: 550
      values: 580
      values: 600
      values: 630
      values: 660
      values: 690
      values: 720
      values: 750
      values: 790
      values: 920
      values: 960
      values: 1200
      values: 1430
      values: 1690
      values: 1770
      values: 1990
      values: 2140
      values: 2260
      values: 2400
      values: 2550
      values: 2610
      values: 2680
      values: 2750
      values: 2820
      values: 2880
      values: 3090
      values: 3350
      values: 3550
      values: 3710
      values: 3820
      values: 3970
      values: 4120
      values: 4260
      values: 4290
      values: 4400
      values: 4550
      values: 4620
      values: 4680
      values: 4710
      values: 4750
      values: 4790
      values: 4830
      values: 4870
      values: 4900
      values: 4980
archive type: LakeSediment
data set name: LakeWA01.Ravindra.2009
dataset id: LCad85043fd257004e193465576d7974b9
created by: github.com/nickmckay/LegacyClimate2LiPD
original data source: Neotoma
legacy climate site id: 24070
legacy climate dataset id: 41864
ages per kyr: NA
max year: 10440
min year: -60
original data url: https://doi.org/10.1594/10.1594/PANGAEA.930512
lipdverse link: https://lipdverse.org/data/LCad85043fd257004e193465576d7974b9/1_0_7
dataset version: 1.0.7
lipd version: 1.3
pub: A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada.

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: 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: 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

compilation name: LegacyClimate-LiPD
compilation version: 0_0_2

t sid: lcR0t3sAT5szANuEclS
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: -60
values: -50
values: -40
values: -30
values: -20
values: -10
values: 0
values: 10
values: 30
values: 60
values: 80
values: 110
values: 140
values: 160
values: 190
values: 220
values: 240
values: 270
values: 300
values: 330
values: 360
values: 390
values: 420
values: 480
values: 500
values: 530
values: 550
values: 580
values: 610
values: 640
values: 660
values: 690
values: 720
values: 750
values: 780
values: 900
values: 930
values: 1210
values: 1470
values: 1730
values: 1800
values: 2010
values: 2140
values: 2270
values: 2400
values: 2530
values: 2600
values: 2660
values: 2730
values: 2800
values: 2860
values: 3060
values: 3330
values: 3550
values: 3730
values: 3830
values: 3980
values: 4120
values: 4260
values: 4290
values: 4400
values: 4540
values: 4610
values: 4670
values: 4710
values: 4740
values: 4780
values: 4820
values: 4860
values: 4900
values: 4980

t sid: lcR0z6byeKnomhjv1tx
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: 0.5
values: 1.5
values: 2.5
values: 3.5
values: 4.5
values: 5.5
values: 6.5
values: 7.5
values: 8.5
values: 9.5
values: 10.5
values: 11.5
values: 12.5
values: 13.5
values: 14.5
values: 15.5
values: 16.5
values: 17.5
values: 18.5
values: 19.5
values: 20.5
values: 21.5
values: 22.5
values: 23.5
values: 24.5
values: 25.5
values: 26.5
values: 27.5
values: 28.5
values: 29.5
values: 30.5
values: 31.5
values: 33.5
values: 34.5
values: 35.5
values: 36.5
values: 37.5
values: 38.5
values: 39.5
values: 40.5
values: 41.5
values: 42.5
values: 43.5
values: 44.5
values: 48.5
values: 49.5
values: 56.5
values: 60.5
values: 64.5
values: 65.5
values: 68.5
values: 70.5
values: 72.5
values: 74.5
values: 76.5
values: 77.5
values: 78.5
values: 79.5
values: 80.5
values: 81.5
values: 84.5
values: 88.5
values: 92.5
values: 97.5
values: 100.5
values: 104.5
values: 108.5
values: 112.5
values: 113.5
values: 116.5
values: 120.5
values: 122.5

t sid: lcRBUQS8kdbl9IOGHfr
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 13.9302
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: 13.6
values: 13.4
values: 12.6
values: 13.3
values: 13.7
values: 14.2
values: 15.1
values: 13.9
values: 14.6
values: 12.8
values: 14.8
values: 12.9
values: 13.2
values: 14
values: 13.8
values: 14.3
values: 12.4
values: 12.5
values: 13.5
values: 15
values: 13.1
values: 14.5
values: 15.2
values: 14.1
values: 12.3
values: 14.9
values: 15.4
values: 13
values: 14.7
values: 12.1
values: 14.4
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRyZkdjY6gA9pvlIdZ
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 2.2425
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 2.24
values: 2.25
values: 2.26
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: WA-PLS
  target: all

t sid: lcRDsQI4d9Vj9NmLyO4
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 13.9198
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: 13.1
values: 13.5
values: 15
values: 13.3
values: 14.3
values: 14.2
values: 13.4
values: 14.4
values: 14
values: 12.8
values: 13.6
values: 14.1
values: 12.6
values: 14.5
values: 12.9
values: 14.9
values: 12.3
values: 14.6
values: 13
values: 14.8
values: 13.2
values: 13.9
values: 13.7
values: 15.1
values: 13.8
values: 15.4
values: 14.7
values: 15.2
values: 15.5
values: 15.6
values: 11.8
values: 12.1
values: 15.7
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcRaBtvhnbXzd6pYLOD
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.8194
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.74
values: 1.81
values: 1.73
values: 1.82
values: 1.78
values: 1.86
values: 1.8
values: 1.88
values: 1.84
values: 1.77
values: 1.85
values: 1.83
values: 1.76
values: 1.75
values: 1.79
values: 1.7
values: 1.71
values: 1.9
values: 1.69
values: 1.87
values: 1.68
values: 1.72
values: 1.95
values: 2.35
values: 2.07
values: 2.09
values: 1.97
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Jul
  direction: positive
  seasonality general: summer+
calibration:
  method: MAT
  target: all

t sid: lcRqPq0E2ipc9svss1o
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: -4.3087
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: -4.2
values: -4.7
values: -6.2
values: -3.9
values: -4.3
values: -3
values: -3.5
values: -5.1
values: -3.7
values: -3.1
values: -2.7
values: -4.4
values: -5.9
values: -6.4
values: -4.1
values: -4.5
values: -4
values: -6.5
values: -5.5
values: -2.2
values: -3.6
values: -5
values: -2.8
values: -4.6
values: -4.9
values: -5.8
values: -2.6
values: -3.3
values: -1.7
values: -3.8
values: -6.6
values: -2.5
values: -3.2
values: -6.1
values: -5.2
values: -5.4
values: -2.1
values: -4.8
values: -5.3
values: -7.5
values: -6.3
values: -1.4
values: -3.4
values: -6
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRg28xetE4FcERjdJy
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 3.0396
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 3.04
values: 3.03
values: 3.05
values: 3.08
values: 3.06
values: 3.07
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcR7wdiBBdrwSVan3v6
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: -4.2865
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: -4.6
values: -5
values: -5.5
values: -4.4
values: -5.4
values: -4.5
values: -3.8
values: -5.3
values: -4.2
values: -4.7
values: -4
values: -5.2
values: -3.3
values: -4.8
values: -2.8
values: -4.3
values: -3.2
values: -5.9
values: -4.9
values: -3.6
values: -3.9
values: -5.6
values: -4.1
values: -5.7
values: -5.1
values: -3.5
values: -2.6
values: -2.5
values: -3.1
values: -3.7
values: -3.4
values: -8
values: -2.2
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRKnRU8BaG89LhHfcI
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 2.0814
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 2.17
values: 2.08
values: 2.04
values: 1.98
values: 2.12
values: 2.1
values: 2.11
values: 2.09
values: 2.13
values: 2.03
values: 2.05
values: 2
values: 2.22
values: 2.07
values: 2.15
values: 2.02
values: 2.16
values: 2.31
values: 2.19
values: 1.99
values: 2.18
values: 2.24
values: 1.96
values: 2.14
values: 2.01
values: 1.95
values: 1.94
values: 2.28
values: 2.78
values: 2.06
values: 2.21
values: 2.42
interpretation:
  scope: climate
  variable: temperature
  variable detail: air@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: MAT
  target: all

t sid: lcRcxrVNR2nWomdDibe
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 310.1524
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
notes: null
values: 332.6
values: 312.1
values: 345.2
values: 366.8
values: 332.8
values: 359.4
values: 330.3
values: 289.2
values: 378
values: 320.2
values: 353.3
values: 309.2
values: 348.6
values: 323.8
values: 283
values: 318.2
values: 368.4
values: 296.6
values: 284.4
values: 356.1
values: 339.6
values: 277.2
values: 327.1
values: 273.6
values: 408.8
values: 322.4
values: 348.1
values: 249.1
values: 268.4
values: 353.2
values: 352.4
values: 336.1
values: 299.5
values: 323.4
values: 319.6
values: 355.3
values: 293.4
values: 287.4
values: 342.3
values: 367.9
values: 366.1
values: 312.6
values: 421.5
values: 364.9
values: 329.5
values: 348.3
values: 325.5
values: 229.3
values: 252.4
values: 290.1
values: 382.5
values: 337.6
values: 340.7
values: 317.1
values: 286.7
values: 331.2
values: 538.7
values: 297.4
values: 184.2
values: 259.8
values: 283.8
values: 276
values: 324.3
values: 309.7
values: 315.9
values: 318.1
values: 291.2

t sid: lcRt2tvSndxaHJf95q1
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 353.238
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 353.05
values: 352.93
values: 353.25
values: 352.99
values: 353.11
values: 353.08
values: 353.33
values: 353.35
values: 353.13
values: 353.14
values: 353.24
values: 353.15
values: 353.31
values: 353.2
values: 353.01
values: 353.07
values: 353.04
values: 353.4
values: 353.55
values: 353.54
values: 353.91
values: 353.23
values: 353.66
values: 353.17
values: 353.53
values: 352.97
values: 352.94
values: 353.19
values: 353.26
values: 352.92
values: 353.37
values: 353.57
values: 353.41
values: 353.52
values: 353.3
values: 353.34
values: 353.09
values: 354.19
values: 353.42
values: 353.1
values: 353.28
values: 353.18
values: 353.79
values: 353.43
values: 352.89
values: 353.36
values: 353.27
values: 353.44
values: 352.96
values: 353.38
values: 353.02
values: 353.85
values: 353.87
values: 354.58
values: 353.12
values: 353.56
values: 353.48
values: 353.29
values: 352.9
values: 352.98
values: 353.51
interpretation:
  scope: climate
  variable: precipitation
  variable detail: precipitation@surface
  seasonality: Annual
  direction: positive
  seasonality general: Annual
calibration:
  method: WA-PLS
  target: all

t sid: lcRey1szXCIV3MDlOQu
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 322.8286
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
notes: null
values: 309.4
values: 300.5
values: 302.2
values: 334.6
values: 303.6
values: 303.1
values: 302.5
values: 313.8
values: 307
values: 304.2
values: 293.6
values: 311.9
values: 298.2
values: 321.6
values: 329.6
values: 316.2
values: 316.8
values: 296.4
values: 320.5
values: 333.9
values: 325.5
values: 289.3
values: 326.3
values: 333.5
values: 331.6
values: 320.2
values: 327.8
values: 315.4
values: 342.2
values: 335.6
values: 332.6
values: 307.5
values: 295.7
values: 326.7
values: 316.3
values: 329
values: 345.1
values: 314.4
values: 320.1
values: 316.9
values: 303.5
values: 329.9
values: 312.6
values: 321.4
values: 316.1
values: 312.4
values: 308.2
values: 335.3
values: 298.5
values: 322.7
values: 330.5
values: 306.7
values: 313.9
values: 336.6
values: 354.4
values: 332
values: 318.4
values: 328.3
values: 325.1
values: 330
values: 311.7
values: 313.4
values: 319.8
values: 328.1
values: 292.4
values: 327.9
values: 315.9

t sid: lcRz8WFv2GH7NS4KdOU
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 264.6567
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 264.85
values: 264.52
values: 264.22
values: 264.31
values: 264.38
values: 264.44
values: 264.3
values: 264.39
values: 264.43
values: 264.13
values: 264.41
values: 264.37
values: 264.46
values: 264.59
values: 264.72
values: 263.84
values: 265.41
values: 264.7
values: 263.96
values: 263.93
values: 264.04
values: 263.74
values: 266.58
values: 264.06
values: 264.45
values: 264.42
values: 263.88
values: 263.91
values: 264.71
values: 263.89
values: 264.73
values: 264.88
values: 265.66
values: 264.76
values: 264.4
values: 264.74
values: 264.35
values: 264.51
values: 263.95
values: 264.24
values: 265.24
values: 263.77
values: 264.02
values: 263.94
values: 264.08
values: 263.81
values: 263.99
values: 263.92
values: 264.18
values: 263.86
values: 263.98
values: 264.07
values: 263.9
values: 264.54
values: 263.69
values: 263.73
values: 263.87
values: 263.62
values: 263.7
values: 264.58
values: 264.77
values: 264.15
values: 264
values: 263.82
values: 264.28
values: 267

t sid: lcRkWs33uxYMlG8FERV
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 14.5635
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: 14.3
values: 14.5
values: 14.6
values: 14.7
values: 14.8
values: 14.1
values: 15
values: 15.1
values: 13.8
values: 15.3
values: 14
values: 14.2
values: 13.7
values: 14.4
values: 14.9
values: 15.2
values: 15.4
values: 13.9
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
in compilation beta:
  compilation name: LegacyClimate-LiPD
  compilation version: 0_0_2

t sid: lcRoeTZpvXUXQDYJbUW
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.1984
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.19
values: 1.2
values: 1.21
values: 1.23
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: lcRDLIrQ3r1bza10EP1
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 258.6143
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
notes: null
values: 302
values: 273.5
values: 272.3
values: 324
values: 292.8
values: 312.5
values: 278.3
values: 240
values: 296.3
values: 271.9
values: 290.6
values: 276.1
values: 299.9
values: 269.9
values: 247.3
values: 238.1
values: 301.6
values: 212.9
values: 243
values: 266.3
values: 242.9
values: 324.9
values: 236.5
values: 308.3
values: 267.1
values: 227.6
values: 261
values: 284
values: 304.3
values: 279.4
values: 264.3
values: 299.2
values: 292
values: 290.8
values: 282.4
values: 294
values: 288.6
values: 298
values: 348.3
values: 302.9
values: 372.9
values: 278.5
values: 336.3
values: 258.1
values: 274.4
values: 260.7
values: 269.7
values: 182.2
values: 226.3
values: 248
values: 287.6
values: 297
values: 276.3
values: 328.6
values: 289.4
values: 359.6
values: 240.7
values: 151.3
values: 188.2
values: 281.9
values: 232.3
values: 290.5
values: 267
values: 291.4
values: 266.9
values: 202.8
values: 251.1

t sid: lcRFSEF4OL5Vk4jFuIE
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 338.5881
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 338.08
values: 338.03
values: 338.51
values: 337.94
values: 338.55
values: 338.24
values: 338.23
values: 338.58
values: 338.79
values: 338.62
values: 338.61
values: 338.09
values: 338.05
values: 338.53
values: 338.68
values: 338.35
values: 338.29
values: 338.43
values: 338.42
values: 337.96
values: 338.16
values: 338.69
values: 339.12
values: 338.84
values: 338.97
values: 339.75
values: 338.14
values: 340.31
values: 338.95
values: 338.27
values: 338.4
values: 338.83
values: 339.17
values: 338.47
values: 338.76
values: 338.72
values: 338.07
values: 338.3
values: 338.93
values: 338.71
values: 338.52
values: 338.96
values: 338.59
values: 338.46
values: 338.44
values: 339.08
values: 339.02
values: 338.37
values: 338.12
values: 338.34
values: 338.48
values: 338.7
values: 338.22
values: 339.43
values: 338.2
values: 338.57
values: 338.77
values: 338.39
values: 338.36
values: 338.88
values: 338.56
values: 338.41
values: 338.5
values: 338.17
values: 338.38
values: 338.86

t sid: lcRXwlNyww6riv4ygrW
variable name: temperature
units: degC
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: -4.6071
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: -4.6
values: -4.8
values: -4.5
values: -4.7
values: -4.4
values: -4.3
values: -4.9
values: -4.1
values: -4.2
values: -5
values: -5.1
values: -5.3
values: -5.2
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
in compilation beta:
  compilation name: LegacyClimate-LiPD
  compilation version: 0_0_2

t sid: lcRloO7sekK2UgRzAN6
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 2.0754
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 2.07
values: 2.08
values: 2.09
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: lcRH5hdhvPNova4q7T8
variable name: precipitation
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 366.7063
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
notes: null
values: 382.9
values: 349.4
values: 371.9
values: 393.5
values: 385.1
values: 383.5
values: 368.6
values: 349.3
values: 378.6
values: 338.4
values: 415.9
values: 384.2
values: 379.4
values: 379.2
values: 439.5
values: 381.2
values: 331.6
values: 298
values: 367
values: 359
values: 334.9
values: 384.6
values: 383.9
values: 436.3
values: 366.5
values: 385.2
values: 377
values: 374.6
values: 422.6
values: 426.1
values: 398.9
values: 377.2
values: 292.8
values: 409.1
values: 376.7
values: 357.7
values: 462.9
values: 390.1
values: 398.2
values: 425.9
values: 391
values: 421.7
values: 430.5
values: 439.6
values: 388.6
values: 317
values: 360.8
values: 384.7
values: 314.1
values: 333
values: 401.7
values: 347.3
values: 329.2
values: 410.6
values: 359.6
values: 424.1
values: 451.3
values: 364
values: 369.8
values: 330.6
values: 313.4
values: 338.2
values: 369.9
values: 316
values: 389.1
values: 398.4
values: 354.4

t sid: lcRACZZn67ECABJEqIp
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 112.5901
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 111.76
values: 111.77
values: 112.04
values: 111.48
values: 112.71
values: 111.82
values: 111.85
values: 111.96
values: 112.81
values: 112.28
values: 114.39
values: 111.7
values: 111.68
values: 114.43
values: 112.64
values: 112.63
values: 111.9
values: 112.19
values: 111.45
values: 112.7
values: 111.98
values: 113.52
values: 114.67
values: 113.64
values: 114.14
values: 112.51
values: 112.79
values: 112.36
values: 122.24
values: 113.18
values: 112.26
values: 112.35
values: 112.68
values: 111.29
values: 112.02
values: 118.22
values: 112.67
values: 112.08
values: 115.42
values: 111.38
values: 112.01
values: 113.6
values: 113.4
values: 111.39
values: 112.38
values: 113.54
values: 111.58
values: 112.53
values: 112.11
values: 112.42
values: 112.15
values: 113.13
values: 111.47
values: 113.35
values: 111.73
values: 112.95
values: 113.56
values: 111.74
values: 112.41
values: 112.33
values: 112.22
values: 112.32
values: 112.09
values: 112.21
values: 111.57
values: 112.76

t sid: lcRut4aNuph5mDCCvOM
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: 14.3706
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: 14
values: 13.7
values: 13.1
values: 14.1
values: 14.2
values: 14.8
values: 15.6
values: 14.6
values: 15.1
values: 14.7
values: 15.5
values: 14.5
values: 13.4
values: 13.5
values: 14.4
values: 14.3
values: 14.9
values: 12.5
values: 15.7
values: 15
values: 15.4
values: 15.2
values: 13.9
values: 15.9
values: 13.3
values: 12.6
values: 13.6
values: 15.8
values: 16
values: 12.4
values: 12.9
values: 13.2
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: lcRkPFrIQCjycIWczXz
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 1.9472
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 1.94
values: 1.95
values: 1.96
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: lcRAaspP4ZPsRPpNmK3
variable name: temperature
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: mean
mean value12k: -3.8127
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
values: -4
values: -4.4
values: -5.7
values: -4.6
values: -3.8
values: -3.6
values: -2.5
values: -3.9
values: -3.2
values: -5
values: -3.5
values: -2.6
values: -2.1
values: -5.8
values: -4.2
values: -6.1
values: -1.4
values: -2.9
values: -2.2
values: -2.4
values: -4.1
values: -5.6
values: -2.7
values: -4.3
values: -3.4
values: -2
values: -2.8
values: -1.8
values: -4.7
values: -3.1
values: -6.2
values: -3.3
values: -2.3
values: -4.8
values: -3.7
values: -5.1
values: -4.5
values: -6.9
values: -1.1
values: -5.2
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: lcRxyCa4XQKzGKkEceF
variable name: uncertainty
units: degC
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 2.7317
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: temperature
notes: NA; paleoData_inferredMaterial has been standardized
values: 2.72
values: 2.73
values: 2.74
values: 2.76
values: 2.75
values: 2.78
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: lcRBEvaydIFwOnSZuma
variable name: precipitation
units: mm/yr
primary timeseries: TRUE
primary age column: false
summary statistic: mean
mean value12k: 362.8762
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained 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: 355.5
values: 342.3
values: 371.3
values: 357.4
values: 336.6
values: 369.6
values: 358.8
values: 357.7
values: 398.6
values: 363.3
values: 355.1
values: 358.3
values: 371.4
values: 379.4
values: 380
values: 389
values: 348.4
values: 360
values: 340
values: 368.3
values: 395.3
values: 335.4
values: 287.5
values: 402
values: 402.2
values: 374.2
values: 411.2
values: 354.5
values: 347.4
values: 407.7
values: 383.4
values: 388.4
values: 323.9
values: 363.9
values: 342
values: 386.8
values: 372.3
values: 311.6
values: 415.5
values: 380.3
values: 411.7
values: 347.9
values: 378
values: 386.4
values: 396.8
values: 367.9
values: 398
values: 366
values: 346.5
values: 367.3
values: 378.4
values: 390.8
values: 348.8
values: 370.2
values: 389.3
values: 354.7
values: 431.4
values: 372.8
values: 362.8
values: 374.9
values: 328.9
values: 337
values: 356.6
values: 362.2
values: 348.1

t sid: lcRdtbiak4cBS9UNCl2
variable name: uncertainty
units: mm/yr
primary timeseries: FALSE
primary age column: false
summary statistic: 1 sigma
mean value12k: 93.6493
median res12k: 60
datum: abs
proxy: pollen
proxy detail: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
proxy general: pollen
inferred material: precipitation
notes: NA; paleoData_inferredMaterial has been standardized
values: 93.48
values: 93.52
values: 93.42
values: 93.47
values: 93.43
values: 93.51
values: 93.68
values: 93.67
values: 93.64
values: 93.39
values: 93.78
values: 93.56
values: 93.53
values: 93.7
values: 93.59
values: 94.03
values: 93.4
values: 93.85
values: 93.94
values: 93.72
values: 93.57
values: 93.8
values: 93.41
values: 94.86
values: 93.69
values: 93.58
values: 94.33
values: 94.2
values: 93.97
values: 93.61
values: 93.74
values: 93.5
values: 93.84
values: 93.62
values: 93.54
values: 93.81
values: 94.27
values: 94.72
values: 94.09
values: 93.6
values: 93.75
values: 93.86
values: 93.44
values: 93.73
values: 93.87
values: 93.93
values: 94
values: 93.46
values: 93.65
values: 93.49
values: 93.63
values: 93.95
values: 95.13
values: 93.9
values: 93.79
values: 93.45
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-chRna5dt7nJRSJNLB1q
    variable name: labID
    units: unitless
    values: NaN
    values: Beta-249092
    values: Beta-249091
    values: Beta-249090
    values: Beta-249089
    values: Beta-249088
    values: Beta-249087
  age type:
    number: 2
    t sid: lc-chRvtGEZEWCP4blYfDU
    variable name: age_type
    units: unitless
    values: Lead-210
    values: Carbon-14
    values: Dates from prior information
  material dated:
    number: 3
    t sid: lc-chR7gd1BJmr70ZHfc6H
    variable name: materialDated
    units: unitless
    values: NaN
    values: Twig
    values: Wood fragments
    values: Wood fragements
  depth:
    number: 4
    t sid: lc-chR46v33sKWyL5FwXsa
    variable name: depth
    units: cm
    values: 0.2
    values: 0.8
    values: 1.2
    values: 1.8
    values: 2.2
    values: 2.8
    values: 3.2
    values: 3.8
    values: 4.2
    values: 4.8
    values: 5.2
    values: 5.8
    values: 6.2
    values: 6.8
    values: 7.2
    values: 7.8
    values: 8.2
    values: 8.8
    values: 9.2
    values: 9.8
    values: 10.2
    values: 10.8
    values: 11.2
    values: 11.8
    values: 12.2
    values: 12.8
    values: 13.2
    values: 13.8
    values: 14.2
    values: 14.8
    values: 15
    values: 55.5
    values: 92.5
    values: 128.5
    values: 189
    values: 208.5
    values: 253
  thickness:
    number: 5
    t sid: lc-chRTWOU5mDvW8YqdnRp
    variable name: thickness
    units: cm
    values: 0.5
    values: 4
    values: NaN
    values: 1
    values: 2
    values: 0
  notes:
    number: 6
    t sid: lc-chRVyh8DGNfEX8RZk2O
    variable name: notes
    units: unitless
    values: NaN
  age14 c:
    number: 7
    t sid: lc-chRBsV9HKTBdLzFXoI3
    variable name: age14C
    units: yr BP 14C
    values: -60
    values: -50
    values: -40
    values: -30
    values: -20
    values: -10
    values: 0
    values: 160
    values: 1150
    values: 3350
    values: 4260
    values: 6470
    values: 7300
    values: 9410
  age:
    number: 8
    t sid: lc-chRQivYd52u6d6ubMz2
    variable name: age
    units: yr BP
    values: -60
    values: -50
    values: -40
    values: -30
    values: -20
    values: -10
    values: 0
    values: 150
    values: 1150
    values: 3580
    values: 4810
    values: 7370
    values: 8110
    values: 10640
  age uncertainty:
    number: 9
    t sid: lc-chRR30FS3JSYQxx5VTN
    variable name: ageUncertainty
    units: yr BP
    summary statistic: 2 sigma
    values: 0
    values: 10
    values: 70
    values: 50
    values: 30
    values: 60
  age14 c uncertainty:
    number: 10
    t sid: lc-chRQlJxcZiLJrhnh3i9
    variable name: age14CUncertainty
    units: yr BP 14C
    summary statistic: 1 sigma
    values: 0
    values: 10
    values: 40
    values: 50
  depth top:
    number: 11
    t sid: lc-chRykaHEpVptse4O6hR
    variable name: depth_top
    units: cm
    values: -0.05
    values: 0.55
    values: 0.95
    values: 1.55
    values: 1.95
    values: 2.55
    values: 2.95
    values: 3.55
    values: 3.95
    values: 4.55
    values: 4.95
    values: 5.55
    values: 5.95
    values: 6.55
    values: 6.95
    values: 7.55
    values: 7.95
    values: 8.55
    values: 8.95
    values: 9.55
    values: 9.95
    values: 10.55
    values: 10.95
    values: 11.55
    values: 11.95
    values: 12.55
    values: 12.95
    values: 13.55
    values: 13.95
    values: 14.55
    values: 13
    values: NaN
    values: 92
    values: 128
    values: 188
    values: 208
    values: 253
  depth bottom:
    number: 12
    t sid: lc-chRw9TPhvAaJdhTQew6
    variable name: depth_bottom
    units: cm
    values: 0.45
    values: 1.05
    values: 1.45
    values: 2.05
    values: 2.45
    values: 3.05
    values: 3.45
    values: 4.05
    values: 4.45
    values: 5.05
    values: 5.45
    values: 6.05
    values: 6.45
    values: 7.05
    values: 7.45
    values: 8.05
    values: 8.45
    values: 9.05
    values: 9.45
    values: 10.05
    values: 10.45
    values: 11.05
    values: 11.45
    values: 12.05
    values: 12.45
    values: 13.05
    values: 13.45
    values: 14.05
    values: 14.45
    values: 15.05
    values: 17
    values: NaN
    values: 93
    values: 129
    values: 190
    values: 209
    values: 253

version: 1.0.7
last version: 1.0.6
curator: nicholas
timestamp: 2023-08-10 23:02:31 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 00:47:11 UTC
changes:
  paleo interpretation metadata: precipitation (lcRBEvaydIFwOnSZuma): 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 17:47:54 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  geographic metadata: geo_elevation: '' has been replaced by '1000'

version: 1.0.4
last version: 1.0.3
curator: nicholas
timestamp: 2023-02-13 23:48:58 UTC
changes:
  paleo interpretation metadata: uncertaintyHigh (lcRBe6MA38yyyZF7q3S): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): interpretation1_scope: '' has been replaced by 'climate'
  paleo column metadata: precipitation (lcRBEvaydIFwOnSZuma): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRcxrVNR2nWomdDibe): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRDLIrQ3r1bza10EP1): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRey1szXCIV3MDlOQu): paleoData_notes: '' has been replaced by 'null'
  paleo column metadata: precipitation (lcRH5hdhvPNova4q7T8): paleoData_notes: '' has been replaced by 'null'

version: 1.0.3
last version: 1.0.2
curator: nicholas
timestamp: 2023-02-09 15:54:36 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  base metadata: archiveType: 'Lake' has been replaced by 'LakeSediment'
  paleo column metadata: age (lcR0t3sAT5szANuEclS): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcR0t3sAT5szANuEclS): paleoData_variableName: 'ageMedian' has been replaced by 'age'
  paleo column metadata: age (lcR0t3sAT5szANuEclS): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: age (lcR0t3sAT5szANuEclS): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: depth (lcR0z6byeKnomhjv1tx): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: depth (lcR0z6byeKnomhjv1tx): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
  paleo column metadata: age (lcR9LOURf4cVBkltT1v): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (lcR9LOURf4cVBkltT1v): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: age (lcR9LOURf4cVBkltT1v): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRaBtvhnbXzd6pYLOD): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRACZZn67ECABJEqIp): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRACZZn67ECABJEqIp): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRACZZn67ECABJEqIp): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRACZZn67ECABJEqIp): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_variableName: 'ageMax' has been replaced by 'uncertaintyHigh'
  paleo column metadata: uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyHigh (lcRBe6MA38yyyZF7q3S): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: precipitation (lcRBEvaydIFwOnSZuma): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_variableName: 'ageMin' has been replaced by 'uncertaintyLow'
  paleo column metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_inferredMaterial: '' has been replaced by 'age'
  paleo column metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): paleoData_isPrimary: '' has been replaced by 'FALSE'
  paleo column metadata: uncertaintyLow (lcRcfqHRUf3HJKYVf6D): 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: precipitation (lcRcxrVNR2nWomdDibe): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: precipitation (lcRDLIrQ3r1bza10EP1): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRdtbiak4cBS9UNCl2): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcRey1szXCIV3MDlOQu): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRg28xetE4FcERjdJy): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRg28xetE4FcERjdJy): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRg28xetE4FcERjdJy): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: precipitation (lcRH5hdhvPNova4q7T8): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRKnRU8BaG89LhHfcI): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRkPFrIQCjycIWczXz): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRkPFrIQCjycIWczXz): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRkPFrIQCjycIWczXz): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRloO7sekK2UgRzAN6): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRloO7sekK2UgRzAN6): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRloO7sekK2UgRzAN6): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRt2tvSndxaHJf95q1): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRt2tvSndxaHJf95q1): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRt2tvSndxaHJf95q1): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRt2tvSndxaHJf95q1): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRxyCa4XQKzGKkEceF): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_variableName: 'temperatureUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_inferredMaterial: '' has been replaced by 'temperature'
  paleo column metadata: uncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo column metadata: uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
  paleo column metadata: uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_variableName: 'precipitationUncertainty' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_inferredMaterial: '' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized'
  paleo interpretation metadata: temperature (lcR7wdiBBdrwSVan3v6): interpretation1_variable: 'T' has been replaced by 'temperature'
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version: 1.0.2
last version: 1.0.1
curator: nicholas
timestamp: 2022-09-09 02:09:55 UTC
changes:
  paleo column metadata: precipitation (lcRBEvaydIFwOnSZuma): 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 (lcRBEvaydIFwOnSZuma): 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 17:35:30 UTC
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  publication metadata: pub2_doi: '' has been replaced by '10.5194/essd-2022-38'
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version: 1.0.0
curator: nicholas
timestamp: 2022-05-26 21:53:11 UTC
notes: Starting the changelog

A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada.
author:
  name: Ravindra, R.
citation: Ravindra, R. (2009)
year: 2009
doi: Ravindra, R., 2009. A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada. Master's thesis. University of Ottawa, Ottawa, Ontario, Canada.
journal: Master's thesis. University of Ottawa

doi: 10.5194/essd-2022-38

longitude: -136.9294
latitude: 61.2444
elevation: 1000
description: The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.
site name: Lake WA01
continent: Western North America
gcmd location: North America>Canada>Yukon Territory