paleo data:
  measurement table:
    table name: paleo1measurement1
    sample ID:
      SISAL entity ID: 563
      has publication: 1
      t sid: S2LRq0DVFOhMeB
      variable name: sampleID
      units: unitless
      description: Refers to the unique identifier for the sample (as given in sample table)
      variable type: sampleMetadata
      mean value12k: 353358
      median res12k: 12.5188
      values: 353219
      values: 353220
      values: 353221
      values: 353222
      values: 353223
      values: 353224
      values: 353225
      values: 353226
      values: 353227
      values: 353228
      values: 353229
      values: 353230
      values: 353231
      values: 353232
      values: 353233
      values: 353234
      values: 353235
      values: 353236
      values: 353237
      values: 353238
      values: 353239
      values: 353240
      values: 353241
      values: 353242
      values: 353243
      values: 353244
      values: 353245
      values: 353246
      values: 353247
      values: 353248
      values: 353249
      values: 353250
      values: 353251
      values: 353252
      values: 353253
      values: 353254
      values: 353255
      values: 353256
      values: 353257
      values: 353258
      values: 353259
      values: 353260
      values: 353261
      values: 353262
      values: 353263
      values: 353264
      values: 353265
      values: 353266
      values: 353267
      values: 353268
      values: 353269
      values: 353270
      values: 353271
      values: 353272
      values: 353273
      values: 353274
      values: 353275
      values: 353276
      values: 353277
      values: 353278
      values: 353279
      values: 353280
      values: 353281
      values: 353282
      values: 353283
      values: 353284
      values: 353285
      values: 353286
      values: 353287
      values: 353288
      values: 353289
    depth:
      SISAL entity ID: 563
      has publication: 1
      t sid: S2LRzeZ6CjoyaD
      variable name: depth
      units: mm
      description: Distance in mm from a reference point
      variable type: measured
      proxy observation type: depth
      is primary: true
      notes: NA; paleoData_isPrimary has been standardized
      values: 0.75
      values: 1.8
      values: 2.85
      values: 3.9
      values: 5.05
      values: 5.6
      values: 6.62
      values: 7.55
      values: 8.58
      values: 9.6
      values: 10.5
      values: 11.64
      values: 12.6
      values: 13.55
      values: 14.5
      values: 15.47
      values: 16.53
      values: 17.5
      values: 18.45
      values: 19.5
      values: 20.52
      values: 21.5
      values: 22.44
      values: 23.4
      values: 24.4
      values: 25.4
      values: 26.43
      values: 27.4
      values: 28.47
      values: 29.42
      values: 30.55
      values: 31.5
      values: 32.4
      values: 33.54
      values: 34.56
      values: 35.58
      values: 36.56
      values: 37.48
      values: 39.02
      values: 40.01
      values: 40.99
      values: 41.9
      values: 42.94
      values: 44.02
      values: 44.85
      values: 45.95
      values: 46.91
      values: 47.92
      values: 48.72
      values: 49.81
      values: 50.83
      values: 51.8
      values: 52.85
      values: 53.8
      values: 54.8
      values: 55.78
      values: 56.78
      values: 57.8
      values: 58.7
      values: 59.8
      values: 60.82
      values: 61.82
      values: 62.8
      values: 63.78
      values: 64.8
      values: 65.78
      values: 66.78
      values: 67.76
      values: 68.69
      values: 69.69
    mineralogy:
      SISAL entity ID: 563
      has publication: 1
      t sid: S2LR7H0xbfGcPs
      variable name: mineralogy
      units: unitless
      description: Description of the mineralogy of the sample
      variable type: measured
      proxy observation type: mineralogy
      median res12k: 12.5188
      mean value12k: NA
      values: calcite
      interpretation:
        scope: climate
      in compilation beta:
        compilation name: SISAL-LiPD
        compilation version: 2_0_0
        compilation version: 2_0_1
    correction:
      SISAL entity ID: 563
      has publication: 1
      t sid: S2LROOW8Z25Uji
      variable name: correction
      units: unitless
      description: Indication of whether the isotope measurements have been corrected in aragonite samples
      variable type: sampleMetadata
      median res12k: 12.5188
      mean value12k: NA
      method: aragonite correction
      notes: NA; paleoData_method has been standardized
      values: not applicable
      interpretation:
        scope: climate
      in compilation beta:
        compilation name: SISAL-LiPD
        compilation version: 2_0_0
        compilation version: 2_0_1
archive type: Speleothem
created by: sisal2lipd
data set name: ElSoplaocave.Rossi.2018
dataset id: qY1riXUUSDxAuiHdlrl9
original data url: https://doi.org/10.17864/1947.256
lipdverse link: https://lipdverse.org/data/qY1riXUUSDxAuiHdlrl9/1_0_11
max year: 14669.7209
min year: 7965.25
ages per kyr: 0
has depth: 1
n unique ages: 0
n unique good ages: 0
n unique other ages: 0
other ages per kyr: 0
lipd version: 1.3
dataset version: 1.0.11
pub: Younger Dryas to Early Holocene paleoclimate in Cantabria (N Spain): Constraints from speleothem Mg, annual fluorescence banding and stable isotope records

scope: climate

compilation name: SISAL-LiPD
compilation version: 2_0_0
compilation version: 2_0_1

compilation name: SISAL-LiPD
compilation version: 2_0_0

direction: negative
variable: precipitation
variable detail: @surface
seasonality general: Annual
scope: climate
seasonality: Annual
variable group: P

compilation name: SISAL-LiPD
compilation version: 2_0_0
compilation version: 2_0_1

compilation name: HoloceneHydroclimate
compilation version: 0_0_2
compilation version: 0_1_0
compilation version: 0_2_0
compilation version: 0_3_0
compilation version: 0_4_0
compilation version: 0_5_0
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

variable: temperature
scope: climate
variable group: Temperature
variable group original: T
variable group direction: negative

compilation name: SISAL-LiPD
compilation version: 2_0_0
compilation version: 2_0_1

compilation name: HoloceneAbruptChange
compilation version: 0_11_0

compilation name: SISAL-LiPD
compilation version: 2_0_0

SISAL entity ID: 563
has publication: 1
t sid: S2LRIixYo5wDj1
variable name: d18O
units: permil
description: Original d18O measurement
variable type: measured
proxy observation type: d18O
notes: "hese authors interpreted the trend as reflecting a general increase in rainfall amounts during the Early Holocene, based on the present-day relationship between rainfall amount and rainwater d18O observed in Cantabria (Comas- Bru and McDermott, 2015; Smith et al., 2016b). The SIR-1 record supports such interpretation. In SIR-1, the increasing d18O trend reversed from ~8.5 to ~8.0 ka. Coevally, both [Mg] and d13C also tend to increase (Fig. 7B), indicating drier conditions. This further sup- ports that the Early Holocene SIR-1 d18O variation mainly responds to variations in the amounts of precipitation." (Rossi et al., 2018)
proxy: d18O
QC certification: CH
mean value12k: -5.092
median res12k: 12.5188
proxy detail: calcite
proxy general: isotope
proxy lumps: isotope
proxy lumps original: d18O
values: -4.6762
values: -4.9887
values: -4.8345
values: -4.9086
values: -5.0699
values: -5.1881
values: -5.2693
values: -5.1641
values: -5.3023
values: -5.1871
values: -5.125
values: -5.1611
values: -5.1961
values: -4.9306
values: -5.0168
values: -5.3334
values: -5.2392
values: -5.3374
values: -5.4797
values: -5.4466
values: -5.4827
values: -5.3584
values: -5.2071
values: -5.3895
values: -5.4386
values: -5.1781
values: -5.0809
values: -5.3885
values: -5.4025
values: -5.3013
values: -5.136
values: -5.1951
values: -5.5818
values: -5.4075
values: -5.2492
values: -5.0739
values: -5.6299
values: -5.8333
values: -5.7316
values: -5.7722
values: -5.7101
values: -5.5738
values: -5.7241
values: -5.7041
values: -5.5668
values: -5.2653
values: -5.4516
values: -5.7371
values: -5.6329
values: -5.7792
values: -5.4015
values: -5.3043
values: -5.2011
values: -5.1981
values: -5.3324
values: -5.3634
values: -5.5578
values: -5.4596
values: -5.2793
values: -5.4506
values: -5.5227
values: -5.4035
values: -5.2302

SISAL entity ID: 563
has publication: 1
t sid: S2LRKkXEWkoD8W
variable name: uncertainty
units: permil
description: Laboratory precision on the d18O measurement
variable type: measured
mean value12k: 0.1
median res12k: 12.5188
measurement material: d18O carbonate
method: precision
notes: NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
values: 0.1
interpretation:
  scope: climate
in compilation beta:
  compilation name: SISAL-LiPD
  compilation version: 2_0_0
  compilation version: 2_0_1

SISAL entity ID: 563
has publication: 1
t sid: S2LRoirhWsuhDY
variable name: uncertainty
units: unitless
description: Description of isotopic standard used
variable type: sampleMetadata
median res12k: 12.5188
mean value12k: NA
measurement material: d18O carbonate
method: standard
notes: NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
values: Vienna-PDB
interpretation:
  scope: climate
in compilation beta:
  compilation name: SISAL-LiPD
  compilation version: 2_0_0
  compilation version: 2_0_1

SISAL entity ID: 563
has publication: 1
t sid: S2LRAXA3YOxDUQ
variable name: d13C
units: permil
description: Original d13C measurement
variable type: measured
proxy observation type: d13C
notes: "Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al., 2018)
QC certification: CH
mean value12k: -7.2114
median res12k: 12.5188
proxy general: isotope
values: -6.0529
values: -6.5826
values: -6.3446
values: -6.4321
values: -6.6121
values: -6.4451
values: -7.0646
values: -6.7135
values: -6.7394
values: -6.8388
values: -6.7046
values: -6.6976
values: -6.7971
values: -6.7493
values: -6.803
values: -6.9572
values: -6.8239
values: -7.3171
values: -7.697
values: -7.2306
values: -6.9602
values: -6.808
values: -6.7911
values: -6.7026
values: -6.9482
values: -6.8587
values: -6.5107
values: -6.9144
values: -7.2963
values: -7.2167
values: -7.2376
values: -7.6761
values: -7.8452
values: -7.7984
values: -7.5319
values: -6.8597
values: -6.5654
values: -6.9731
values: -6.9552
values: -7.1262
values: -7.0407
values: -7.6194
values: -7.5299
values: -7.7467
values: -8.0261
values: -7.9108
values: -7.0695
values: -8.1047
values: -7.8303
values: -7.7099
values: -7.9327
values: -8.2946
values: -7.3758
values: -6.8766
values: -7.0039
values: -6.8806
values: -7.2028
values: -6.9104
values: -7.0258
values: -7.1352
values: -7.4265
values: -7.0944
values: -7.3897
values: -7.3072
values: -7.4603
values: -7.336
values: -7.2416

SISAL entity ID: 563
has publication: 1
t sid: S2LRMZgbVDudjp
variable name: uncertainty
units: permil
description: Laboratory precision on the d13C measurement
variable type: measured
mean value12k: 0.1
median res12k: 12.5188
measurement material: d13C
method: precision
notes: NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
values: 0.1
interpretation:
  scope: climate
in compilation beta:
  compilation name: SISAL-LiPD
  compilation version: 2_0_0
  compilation version: 2_0_1

SISAL entity ID: 563
has publication: 1
t sid: S2LRsRGWDu4Rd6
variable name: uncertainty
units: unitless
description: Description of isotopic standard used
variable type: sampleMetadata
median res12k: 12.5188
mean value12k: NA
measurement material: d13C
method: standard
notes: NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
values: Vienna-PDB
interpretation:
  scope: climate
in compilation beta:
  compilation name: SISAL-LiPD
  compilation version: 2_0_0
  compilation version: 2_0_1

SISAL entity ID: 563
has publication: 1
t sid: S2LRmVXKEwajmg
variable name: age
units: yr BP
description: Original published calibrated age of the sample in years BP
variable type: inferred
inferred variable type: age
primary age column: true
units original: yr BP
datum: 1950
is primary: true
notes: NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
values: 7965.25
values: 7991.6
values: 8019.25
values: 8045.75
values: 8073.6
values: 8090.3333
values: 8106.6667
values: 8119.8333
values: 8130.3
values: 8143.2857
values: 8154.125
values: 8165.2
values: 8175
values: 8182.1667
values: 8192.4444
values: 8204.1667
values: 8213.8571
values: 8228
values: 8238.5
values: 8248.5833
values: 8258.3
values: 8272.6667
values: 8285.2857
values: 8302.2857
values: 8314.2222
values: 8331.1667
values: 8350
values: 8371.3333
values: 8389.7143
values: 8398.0526
values: 8409.2308
values: 8416.8
values: 8422.2
values: 8440.4
values: 8453.7143
values: 8465.7778
values: 8479.4286
values: 8494.5
values: 8516.75
values: 8526.2
values: 8535.3571
values: 8547.75
values: 8553.8333
values: 8561
values: 8565.7857
values: 8576.5
values: 8585.2
values: 8597.3077
values: 8604.0714
values: 8614.3636
values: 8623.3571
values: 8627.9091
values: 8639.25
values: 8653
values: 8663
values: 8673.5833
values: 8682.7143
values: 8692.1429
values: 8701.1429
values: 8713
values: 8725.2222
values: 8735.2857
values: 8752.5556
values: 8760.7778
values: 8773.5
values: 8788.7143
values: 8800

measurement table:
  table name: chron1measurement1
  sisal dating id:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRdEGdUrxPg7
    variable name: sisalDatingId
    units: unitless
    description: Unique identifier for each date
    variable type: sampleMetadata
    number: 1
    values: 10071
    values: 10072
    values: 10073
    values: 10074
    values: 10075
    values: 10076
    values: 10077
    values: 10078
    values: 10079
    values: 10080
    values: 10081
    values: 10082
    values: 10083
    values: 10084
    values: 10085
    values: 10086
    values: 10087
    values: 10088
    values: 10089
    values: 10090
    values: 10091
    values: NA
  material dated:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRPmIm9j7O5R
    variable name: materialDated
    units: unitless
    description: Mineralogy of the dated sample
    variable type: sampleMetadata
    number: 2
    values: calcite
  retained:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRbfouGAtZTS
    variable name: retained
    units: unitless
    description: Indication of whether the date is used in the original age model (opposite of rejected)
    variable type: sampleMetadata
    number: 3
    values: yes
    values: no
  th232:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRpfUDjZsLxG
    variable name: Th230/Th232
    units: unitless
    description: 230Th/232Th activity ratio of the dated sample
    variable type: measured
    proxy observation type: Th230/Th232
    number: 4
    values: 78
    values: 132.8
    values: 235.9
    values: 28.49
    values: 111.8
    values: 88.69
    values: 477.5
    values: 328.3
    values: 711
    values: 201.4
    values: 217.7
    values: 33.6
    values: 61
    values: 272.2
    values: 243.9
    values: 480.5
    values: 221.6
    values: 322.7
    values: 466.8
    values: NA
  U238:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcR6xrOXeOGhd
    variable name: Th230/U238
    units: unitless
    description: 230Th/238U activity ratio of the dated sample
    variable type: measured
    proxy observation type: Th230/U238
    number: 5
    values: 0.0987
    values: 0.1012
    values: 0.1193
    values: 0.1179
    values: 0.1041
    values: 0.1091
    values: 0.1174
    values: 0.1256
    values: 0.1274
    values: 0.137
    values: 0.1388
    values: 0.1423
    values: 0.1489
    values: 0.159
    values: 0.1546
    values: 0.1563
    values: 0.1558
    values: 0.1611
    values: 0.1707
    values: NA
  U238 uncertainty:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRalyn9HbENL
    variable name: Th230/U238Uncertainty
    units: unitless
    description: 230Th/238U activity ratio 2-sigma uncertainty of the dated sample
    variable type: measured
    number: 6
    values: 0.0025
    values: 0.001
    values: 0.0023
    values: 0.0015
    values: 0.002
    values: 0.0022
    values: 0.0018
    values: 0.0014
    values: 0.0017
    values: 0.0013
    values: 0.0029
    values: 0.0021
    values: 0.0016
    values: NA
  U238:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRpQfxvPPEzn
    variable name: U234/U238
    units: unitless
    description: 234U/238U activity ratio of the dated sample
    variable type: measured
    proxy observation type: U234/U238
    number: 7
    values: 1.3443
    values: 1.3424
    values: 1.3287
    values: 1.3371
    values: 1.3317
    values: 1.3314
    values: 1.3459
    values: 1.3454
    values: 1.3307
    values: 1.3526
    values: 1.3687
    values: 1.3619
    values: 1.3678
    values: 1.3774
    values: 1.3627
    values: 1.3725
    values: 1.3705
    values: 1.3669
    values: 1.356
    values: NA
  U238 uncertainty:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRUZevS5d6dS
    variable name: U234/U238Uncertainty
    units: unitless
    description: 234U/238U activity ratio 2-sigma uncertainty of the dated sample
    variable type: measured
    number: 8
    values: 0.0061
    values: 0.0054
    values: 0.0041
    values: 0.0081
    values: 0.006
    values: 0.0069
    values: 0.0049
    values: 0.0057
    values: 0.0037
    values: 0.0076
    values: 0.0059
    values: 0.0029
    values: 0.0032
    values: 0.0067
    values: 0.008
    values: 0.0079
    values: 0.0062
    values: 0.0078
    values: 0.004
    values: NA
  decay constant:
    SISAL entity ID: 563
    has publication: 1
    t sid: S2LcRc5d5FDAwHX
    variable name: decayConstant
    units: unitless
    description: Description of the half-life used for 230Th and 234U for U/Th samples
    variable type: sampleMetadata
    number: 9
    values: Cheng et al. 2013

SISAL entity ID: 563
has publication: 1
variable name: age_type
t sid: S2LcRIsVGuQfCWr
units: unitless
description: broad class of age control
variable type: sampleMetadata
variable name original: ageType
number: 10
values: U/Th
values: layerCount

version: 1.0.11
last version: 1.0.10
curator: nicholas
timestamp: 2023-08-10 22:49:03 UTC
changes:
  base metadata: originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'
  publication metadata: pub1_author: '' has been replaced by 'Carlos Rossi and Petra Bajo and Rafael P. Lozano and John Hellstrom'
  publication metadata: pub1_journal: '' has been replaced by 'Quaternary Science Reviews'
  publication metadata: pub1_pages: '' has been replaced by '71--85'
  publication metadata: pub1_title: '' has been replaced by 'Younger Dryas to Early Holocene paleoclimate in Cantabria (N Spain): Constraints from speleothem Mg, annual fluorescence banding and stable isotope records'

version: 1.0.10
last version: 1.0.9
curator: nicholas
timestamp: 2023-05-12 21:53:52 UTC
changes:
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_notes: '((( "Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 �� 0.14 to 11.62 �� 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al., 2018) ))) "Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al…

version: 1.0.9
last version: 1.0.8
curator: nicholas
timestamp: 2023-02-13 23:41:41 UTC
changes:
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_notes: '"Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al., 2018)' has been replaced by '((( "Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 �� 0.14 to 11.62 �� 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional tempera…

version: 1.0.8
last version: 1.0.7
curator: nicholas
timestamp: 2023-02-09 15:39:52 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
  geographic metadata: geo_elevation: '' has been replaced by '550'
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_variable: 'T' has been replaced by 'temperature'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_variable: 'P' has been replaced by 'precipitation'
  paleo column metadata: uncertainty (S2LRKkXEWkoD8W): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
  paleo column metadata: uncertainty (S2LRKkXEWkoD8W): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (S2LRKkXEWkoD8W): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
  paleo column metadata: uncertainty (S2LRKkXEWkoD8W): paleoData_method: '' has been replaced by 'precision'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_units: 'BP' has been replaced by 'yr BP'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_datum: '' has been replaced by '1950'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_isPrimary: '' has been replaced by 'TRUE'
  paleo column metadata: uncertainty (S2LRMZgbVDudjp): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
  paleo column metadata: uncertainty (S2LRMZgbVDudjp): paleoData_variableName: 'd13CPrecision' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (S2LRMZgbVDudjp): paleoData_measurementMaterial: '' has been replaced by 'd13C'
  paleo column metadata: uncertainty (S2LRMZgbVDudjp): paleoData_method: '' has been replaced by 'precision'
  paleo column metadata: uncertainty (S2LRoirhWsuhDY): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
  paleo column metadata: uncertainty (S2LRoirhWsuhDY): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (S2LRoirhWsuhDY): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
  paleo column metadata: uncertainty (S2LRoirhWsuhDY): paleoData_method: '' has been replaced by 'standard'
  paleo column metadata: correction (S2LROOW8Z25Uji): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
  paleo column metadata: correction (S2LROOW8Z25Uji): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
  paleo column metadata: correction (S2LROOW8Z25Uji): paleoData_method: '' has been replaced by 'aragonite correction'
  paleo column metadata: sampleID (S2LRq0DVFOhMeB): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
  paleo column metadata: uncertainty (S2LRsRGWDu4Rd6): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
  paleo column metadata: uncertainty (S2LRsRGWDu4Rd6): paleoData_variableName: 'd13CStandard' has been replaced by 'uncertainty'
  paleo column metadata: uncertainty (S2LRsRGWDu4Rd6): paleoData_measurementMaterial: '' has been replaced by 'd13C'
  paleo column metadata: uncertainty (S2LRsRGWDu4Rd6): paleoData_method: '' has been replaced by 'standard'
  paleo column metadata: depth (S2LRzeZ6CjoyaD): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
  paleo column metadata: depth (S2LRzeZ6CjoyaD): paleoData_units: 'depth_sample' has been replaced by 'mm'
  paleo column metadata: depth (S2LRzeZ6CjoyaD): paleoData_isPrimary: '' has been replaced by 'TRUE'

version: 1.0.7
last version: 1.0.6
curator: nicholas
timestamp: 2022-07-28 17:30:40 UTC
changes:
  geographic metadata: geo_elevation: '550' has been replaced by ''

version: 1.0.6
last version: 1.0.5
curator: nicholas
timestamp: 2022-07-15 23:00:39 UTC
changes:
  paleo interpretation metadata: mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: '' has been replaced by 'climate'

version: 1.0.5
last version: 1.0.4
curator: nicholas
timestamp: 2022-05-18 00:25:36 UTC
changes:
  paleo interpretation metadata: mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroup: '' has been replaced by 'Temperature'
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroupDirection: '' has been replaced by 'negative'
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_variableGroupOriginal: '' has been replaced by 'T'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_variableGroup: '' has been replaced by 'P'
  paleo interpretation metadata: d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: 'climate' has been replaced by ''
  paleo interpretation metadata: d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: 'climate' has been replaced by ''
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_proxyLumps: '' has been replaced by 'isotope'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_units: 'yr BP' has been replaced by 'BP'
  paleo column metadata: age (S2LRmVXKEwajmg): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
  chron column metadata: age_type (S2LcRIsVGuQfCWr): chronData_variableName: 'ageType' has been replaced by 'age_type'
  chron column metadata: age_type (S2LcRIsVGuQfCWr): chronData_variableNameOriginal: '' has been replaced by 'ageType'

version: 1.0.4
last version: 1.0.3
curator: nicholas
timestamp: 2021-10-05 21:39:11 UTC
changes:
  geographic metadata: geo_gcmdLocation: '' has been replaced by 'Europe>Southern Europe>Spain'

version: 1.0.3
last version: 1.0.2
curator: nick
timestamp: 2021-04-13 02:31:54 UTC
changes:
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,643' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'

version: 1.0.2
last version: 1.0.1
curator: nick
timestamp: 2021-03-17 01:52:59 UTC
changes:
  base metadata: archiveType: 'speleothem' has been replaced by 'Speleothem'
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_notes: '"Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al., 2018)' has been replaced by '"Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on Speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature."…
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_proxyGeneral: '' has been replaced by 'isotope'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_seasonality: '' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,643'

version: 1.0.1
last version: 1.0.0
curator: nick
timestamp: 2021-01-12 02:28:50 UTC
changes:
  paleo interpretation metadata: mineralogy (S2LR7H0xbfGcPs): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13C (S2LRAXA3YOxDUQ): interpretation1_variable: '' has been replaced by 'T'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_direction: '' has been replaced by 'negative'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_variable: '' has been replaced by 'P'
  paleo interpretation metadata: d18O (S2LRIixYo5wDj1): interpretation1_variableDetail: '' has been replaced by '@surface'
  paleo interpretation metadata: d18OPrecision (S2LRKkXEWkoD8W): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13CPrecision (S2LRMZgbVDudjp): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d18OStandard (S2LRoirhWsuhDY): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: hasAragoniteCorrection (S2LROOW8Z25Uji): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: sisalSampleID (S2LRq0DVFOhMeB): interpretation1_scope: '' has been replaced by 'climate'
  paleo interpretation metadata: d13CStandard (S2LRsRGWDu4Rd6): interpretation1_scope: '' has been replaced by 'climate'
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_notes: '' has been replaced by '"Also, SIR-1 growth rate is much reduced in periods of high d13C. Given the strong temperature control on speleothem growth rates (Borsato et al., 2016), such relationship is consistent with reduced soil productivity during colder periods....colder intervals limited soil pro- ductivity and dripwater availability, leading to higher d13C and [Mg], reduced growth rate, and poor or null development of fluo- rescent lamination. Conversely, relatively warm and humid cli- mates favored forest development and resulted in higher growth rates, lower d13C and [Mg], and well developed annual fluorescent lamination...As recorded by SIR-1 and other stalagmites of the region, the YD is marked by a prominent positive d13C excursion whose chronol- ogy (12.95 ± 0.14 to 11.62 ± 0.16 ka) closely matches the YD as defined in Greenland ice, supporting a high YD synchronicity and the sensitivity of stalagmitic d13C in this region to changes in regional temperature." (Rossi et al., 2018)'
  paleo column metadata: d13C (S2LRAXA3YOxDUQ): paleoData_QCCertification: '' has been replaced by 'CH'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_notes: '' has been replaced by '"hese authors interpreted the trend as reflecting a general increase in rainfall amounts during the Early Holocene, based on the present-day relationship between rainfall amount and rainwater d18O observed in Cantabria (Comas- Bru and McDermott, 2015; Smith et al., 2016b). The SIR-1 record supports such interpretation. In SIR-1, the increasing d18O trend reversed from ~8.5 to ~8.0 ka. Coevally, both [Mg] and d13C also tend to increase (Fig. 7B), indicating drier conditions. This further sup- ports that the Early Holocene SIR-1 d18O variation mainly responds to variations in the amounts of precipitation." (Rossi et al., 2018)'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_proxy: '' has been replaced by 'd18O'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_proxyDetail: '' has been replaced by 'calcite'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_proxyGeneral: '' has been replaced by 'isotope'
  paleo column metadata: d18O (S2LRIixYo5wDj1): paleoData_QCCertification: '' has been replaced by 'CH'

version: 1.0.0
curator: nick
timestamp: 2020-09-29 14:29:26 UTC
notes: Created from SISALv2

Younger Dryas to Early Holocene paleoclimate in Cantabria (N Spain): Constraints from speleothem Mg, annual fluorescence banding and stable isotope records
author:
  name: Carlos Rossi and Petra Bajo and Rafael P. Lozano and John Hellstrom
citation: Rossi, C., Bajo, P., Lozano, R. P. and Hellstrom, J.: Younger Dryas to Early Holocene paleoclimate in Cantabria (N Spain): Constraints from speleothem Mg, annual fluorescence banding and stable isotope records, Quat. Sci. Rev., 192, 71<96>85, 2018.
year: 2018
doi: 10.1016/j.quascirev.2018.05.025
journal: Quaternary Science Reviews
pages: 71--85

longitude: -4.3937
latitude: 43.2962
elevation: 550
site name: El Soplao cave
sisal site id: 261
geology: dolomite
rock age: Cretaceous
has monitoring: yes
gcmd location: Europe>Southern Europe>Spain