# Lake Imandra, Russia Biomarker, Geochemistry, Magnetic Susceptibility, Foraminifer, and Pollen Data over the last 11,000 years #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/40079 # Landing_Page_Description: NOAA Landing Page of this data file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-lake-40079.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Paleolimnology # # Dataset_DOI: 10.25921/nbsb-aw05 # # Science_Keywords: #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/paleolimnology/asia/russia/holtzman2024/holtzman2024-toc-grain.txt # Data_Download_Description: NOAA Template File; Lake Imandra TOC and Grain Size Data # #------------------ # Contribution_Date # Date: 2024-11-26 #------------------ # File_Last_Modified_Date # Date: 2025-04-03 #------------------ # Title # Study_Name: Lake Imandra, Russia Biomarker, Geochemistry, Magnetic Susceptibility, Foraminifer, and Pollen Data over the last 11,000 years #------------------ # Investigators # Investigators: Holtzman, Hannah; Thomas, Elizabeth; Erb, Michael; Marshall, Leah; Castañeda, Isla; Kaufman, Darrell; McKay, Nicholas; Melles, Martin #------------------ # Description_Notes_and_Keywords # Description: #------------------ # Publication # Authors: Holtzman, Hannah; Thomas, Elizabeth; Erb, Michael; Marshall, Leah; Castañeda, Isla; Kaufman, Darrell; McKay, Nicholas; Melles, Martin # Published_Date_or_Year: 2025 # Published_Title: Early Holocene Atmospheric Circulation Changes Over Northern Europe Based on Isotopic and Biomarker Evidence From Kola Peninsula # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 40 # Edition: # Issue: 3 # Pages: # Report_Number: e2024PA005076 # DOI: 10.1029/2024PA005076 # Online_Resource: # Full_Citation: # Abstract: Rapid Arctic warming this century will likely cause major water cycle and atmospheric circulation changes, including weakening mid-latitude westerly winds and more persistent summer high pressures over Fennoscandia. These conditions can cause drought in northern Europe and extreme rainfall in the Mediterranean region. Uncertainties in the spatiotemporal patterns of these predictions can be partially addressed with records of past climate response to rapid change. The early Holocene collapse of the Northern Hemisphere ice sheets provides a natural experiment to evaluate the climate response to rapid changes in boundary conditions. We analyzed lipid biomarker distributions and hydrogen isotope (δ2H) values from Lake Imandra, Kola Peninsula, to infer Holocene summer temperature and summer precipitation δ2H values. Sensitivity tests of a lake model suggest summer precipitation δ2H values are the main mechanism influencing Lake Imandra δ2H values. Summer precipitation isotope values exhibited a nearly 20‰ 2H-depletion between 8.6 and 8.0 ka, with 2H -enriched values before 8.6 ka and 2H -depleted values 8.0 ka to present. Maximum warmth occurred from 8.5 to 7.0 ka. Climate model experiments suggest that the early Holocene Laurentide Ice Sheet collapse caused a westward shift of the Fennoscandian summer high-pressure center. This caused a decrease in the proportion of local, 2H-enriched precipitation falling throughout Fennoscandia and an increase in far-traveled, 2H-depleted precipitation from the mid-latitudes, circulation that persisted throughout the Holocene. These results illustrate the sensitivity of climate in Fennoscandia and show that circulation regime shifts can occur in response to changes in boundary conditions far upwind. #------------------ # Publication # Authors: Lenz, Matthias; Savelieva, Larisa; Frolova, Larisa; Cherezova, Anna; Moros, Matthias; Baumer, Marlene M.; Gromig, Raphael; Kostromina, Natalia; Nigmatullin, Niyaz; Kolka, Vasili; Wagner, Benrd; Fedorov, Grigory; Melles, Martin # Published_Date_or_Year: 2021 # Published_Title: Lateglacial and Holocene environmental history of the central Kola region, northwestern Russia revealed by a sediment succession from Lake Imandra # Journal_Name: Boreas # Volume: 50 # Edition: # Issue: 1 # Pages: 76-100 # Report_Number: # DOI: 10.1111/bor.12465 # Online_Resource: # Full_Citation: # Abstract: #------------------ # Funding_Agency # Funding_Agency_Name: Geological Society of America Quaternary Geology and Geomorphology Division # Grant: Arthur D. Howard Award #------------------ # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: EAR-IF 1652274, ARCSS 1947981, ARCSS 1948005 #------------------ # Funding_Agency # Funding_Agency_Name: US-Norway Fulbright Foundation # Grant: Fulbright Norway Scholar #------------------ # Funding_Agency # Funding_Agency_Name: German Research Foundation # Grant: ME 1169/28 #------------------ # Site_Information # Site_Name: Lake Imandra # Location: Russia # Northernmost_Latitude: 67.7158 # Southernmost_Latitude: 67.7158 # Easternmost_Longitude: 33.0851 # Westernmost_Longitude: 33.0851 # Elevation_m: 127 #------------------ # Data_Collection # Collection_Name: Imandra TOC grainsize Holtzman2024 # First_Year: 11170 # Last_Year: -68 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: physical properties # Notes: #------------------ # Chronology_Information # Chronology: Radiocarbon # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-14c-terms.csv # Chronology_Download_Description: Radiocarbon terms and definitions. # Chronology_Notes: Age-depth constraints from core Co1410. Samples for this study were analyzed at the Arizona Climate and Ecosystems (ACE) Isotope Laboratory at Northern Arizona University # Rejection_Rationale: # Reservoir_Method: # Calibration_Method: Calib8.2 (Stuiver et al., 2022) and IntCal20 (Reimer et al., 2020) # Age_Model_Method: # Missing_Values: # Chronology_Table: # lab_code samp_id depth_end_cm depth_start_cm depth_cm weight_ug age_14C_BP1950 age_14C_1s_yr age_calib_BP1950 age_calib_2s_yr calib_curve # Lenz Surface nan nan 0 nan nan nan -68 1 None # Lenz Co1410_26-28 26 28 27 nan nan nan -36 10 IntCal20 # Lenz Co1410_40-42 40 42 41 nan nan nan 50 10 IntCal20 # 7625.1.1 Co1410-3-I 70cm 70 72 71 56 1104 71 1020 220 IntCal20 # Lenz COL5648.1.0.0.1 104 106 105 27 1398 81 1307 195.5 IntCal20 # 3616.1.1 Co1410-8-I 212-214 cm 212 214 213 98 3006 69 3191 198 IntCal20 # 4752.1.1 Co1410-4-I 258-260 258 260 259 59 4140 84 4667 211.5 IntCal20 # 7626.1.1 Co1410-4-I 274cm 274 276 275 33 4375 87 4991 234.5 IntCal20 # Lenz COL5649.1.0.0.1 332 334 333 28 5227 92 6009 260.5 IntCal20 # 4753.1.1 Co1410-4-II 350-352 350 352 351 84 5763 92 6562 230.5 IntCal20 # 7629.1.1 Co1410-4-I 365cm 364 366 365 99 5865 97 6680 245.5 IntCal20 # 3618.1.1 Co1410-4-II 396-398 cm 396 398 397 90 6647 88 7524 157 IntCal20 # 3617.1.1 Co1410-4-II 396-398 cm 396 398 397 88 6844 88 7687 200 IntCal20 # 3611.1.1 Co1410-9-I 406-408 cm 406 408 407 99 7401 88 8218 171 IntCal20 # 4754.1.1 Co1410-9-I 410-412 410 412 411 92 7425 106 8236 190 IntCal20 # Lenz COL5650.1.0.0.1 412 414 413 31 7080 86 7894 165.5 IntCal20 # 3612.1.1 Co1410-9-I 414-416 cm 414 416 415 96 7273 92 8095 194.5 IntCal20 # 3613.1.1 Co1410-9-I 414-416 cm 414 416 415 93 7364 88 8175 173 IntCal20 # 4755.1.1 Co1410-9-I 418-420 418 420 419 95 7963 107 8817 291 IntCal20 # 3615.1.1 Co1410-9-I 422-424 cm 422 424 423 96 6463 84 7369 195 IntCal20 # 3614.1.1 Co1410-9-I 422-424 cm 422 424 423 95 6877 87 7721 173.5 IntCal20 # 3925.1.1 Co1410-5-I 434-436 434 436 435 93 8042 101 8901 331 IntCal20 # 4756.1.1 Co1410-5-I 438-440 438 440 439 92 7781 109 8583 299 IntCal20 # Lenz COL5291.1.1 448 450 449 997 8017 51 8873 184.5 IntCal20 # 3922.1.1 Co1410-5-I 464-466 464 466 465 94 8398 101 9383 252 IntCal20 # 3923.1.1 Co1410-5-I 488-490 488 490 489 55 8735 99 9761 304 IntCal20 # 7628.1.1 Co1410-5-I 494cm 494 496 495 97 9188 122 10379 371 IntCal20 # 7627.1.1 Co1410-5-I 499cm 498 500 499 93 9181 122 10373 368 IntCal20 # Lenz COL5652.1.0.0.1 504 506 505 31 9769 92 11180 313 IntCal20 # 3926.1.1 Co1410-5-I 505-507 505 507 506 90 9705 111 11056 307.5 IntCal20 # 7630.1.1 Co1410-5-II 508-512cm 508 512 510 91 9623 125 10948 327 IntCal20 # Lenz COL5651.1.0.0.1 510 512 511 36 10032 93 11549 311.5 IntCal20 # 3924.1.1 Co1410-5-II 512-514 512 514 513 99 9623 110 10951 311.5 IntCal20 # 7631.1.1 Co1410-5-II 514-518cm 514 518 516 93 9855 127 11318 505 IntCal20 #------------------ # Variables # # Data variables follow that are preceded by "##" in columns one and two. # Data line variables format: Variables list, one per line, shortname-tab-longname-tab-longname components (10 components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data, additional_information) # ## depth depth,,,centimeter,,paleolimnology,,,N, ## s sulfur,,,percent,,paleolimnology,,,N, ## toc organic carbon,,,percent,,paleolimnology,,,N,total organic carbon ## toc/tn carbon/nitrogen,,,dimensionless,,paleolimnology,,,N,total organic carbon/total nitrogen ## waterContent water content,,,percent,,paleolimnology,,,N,Water wet mass ## d50 grain size parameter,,,micrometer,,paleolimnology,,,N,Median grain size ## em1 grain size parameter,,,micrometer,,paleolimnology,,,N,End member 1 grain size ## em2 grain size parameter,,,micrometer,,paleolimnology,,,N,End member 2 grain size ## em3 grain size parameter,,,micrometer,,paleolimnology,,,N,End member 3 grain size ## ageMedian age,,,calendar year before present,,paleolimnology,,,N,Median of the age ensemble; created by geoChronR::mapEnsembleToPaleoData() # #------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header) # Missing_Values: nan # depth s toc toc/tn waterContent d50 em1 em2 em3 ageMedian 0 0.11 6.02 7.94 80.71 15.67 58.21 33.31 8.49 -68.15125 2 0.15 6.43 8.07 83.19 15.69 56.35 34.41 9.24 -65.28525 4 0.16 5.86 7.67 81.5 15.31 59.88 31.03 9.09 -62.53895 6 0.2 5.89 7.71 80.75 14.48 62.08 28.78 9.14 -59.5260218023762 8 0.24 5.96 7.87 82.35 14.83 62.8 26.85 10.36 -55.4351439251486 10 0.24 5.89 7.92 81 14.63 63.53 26.39 10.08 -52.0963488229703 12 0.32 5.86 8.18 81.46 14.36 63.77 26.07 10.16 -48.4994863081188 14 0.34 5.99 8.34 81.91 14.83 64.58 23.94 11.48 -44.8704348039604 16 0.53 5.47 8.3 82.97 15.09 64.16 23.46 12.38 -41.9495364083168 18 0.5 5.82 7.83 84.42 17.55 61.12 23.21 15.67 -38.8612514522773 20 0.4 5.31 7.94 85.52 15.72 65.86 17.74 16.39 -35.3798101726733 22 0.28 4.31 7.58 82.51 11.37 78.58 5.05 16.38 -32.3517324946535 24 0.3 4.03 7.69 82.94 10.94 78.09 8.14 13.77 -29.3796109805941 26 0.23 4.38 9.15 78.09 10.91 77.04 13.56 9.39 -26.5495620229704 28 0.24 4.58 8.91 79.13 13.66 68.57 20.89 10.54 -18.8217019984555 30 0.26 5.02 9.2 80.21 18.11 54.3 34.34 11.36 -11.0608119081188 32 0.18 5.31 9.21 79.26 19.5 48.56 40.44 11 -3.59973855960366 34 0.17 5.16 9.12 78.62 21.1 48.04 37.64 14.32 7.20430106376275 36 0.16 5.27 8.9 79.03 21.59 46.72 38.22 15.05 16.3578228966338 38 0.14 5.17 8.86 79.08 20.96 46.99 38.96 14.05 27.2799604586141 40 0.14 5.38 9.54 78.78 22.02 47.18 37.05 15.78 41.0816295148517 42 0.14 5.41 8.8 79.22 21.73 46.54 38.35 15.11 60.1208256756443 44 0.14 5.15 8.44 78.43 21.06 47.24 39.56 13.2 110.330769050694 46 0.14 5.18 9.01 78.32 23.01 45.86 37.49 16.65 161.100194553268 48 0.14 5.27 8.75 77.98 21.11 47.88 37.94 14.18 213.289060748516 50 0.14 5 9.16 78.65 20.78 48.11 38.19 13.7 285.414431971089 52 0.14 5.09 9.11 78.52 20.76 48.83 36.86 14.31 338.949329993664 54 0.14 5.3 8.6 80.06 21.21 47.93 37.17 14.9 403.549848344951 56 0.14 5.16 8.77 80.45 21.42 46.22 39.03 14.75 461.477043431287 58 0.14 5.02 8.96 76.73 22.06 44.78 39.58 15.65 517.37681118495 60 0.13 5 8.64 78.74 22.47 44.08 40.28 15.64 573.018759837228 62 0.15 4.91 8.58 80.9 20.27 47.63 39.87 12.5 635.927489112871 64 0.14 4.88 8.94 78.02 20.4 46.41 40.68 12.9 691.420700213509 66 0.15 5.09 8.34 76.54 20.83 46.33 39.74 13.93 745.722190832871 68 0.15 5.17 8.92 78.06 21.37 45.38 39.59 15.03 800.548055433663 70 0.14 5.25 8.97 77.41 20.9 46.88 39.54 13.58 846.285721064554 72 0.17 5.01 8.53 76.11 21.87 47.12 37.24 15.64 888.235922834455 74 0.15 5.25 8.91 77.34 19.83 50.51 37.34 12.15 927.728447198812 76 0.15 5.17 9.11 77.56 19.83 51.05 36.29 12.66 958.390120334257 78 0.16 5.32 8.92 77.13 20.22 48.49 38.65 12.87 984.175822825742 80 0.14 5.41 8.96 77.36 22.17 45.76 38.1 16.14 1011.39201742178 82 0.15 5.5 8.99 78.67 22.61 44.81 38.14 17.05 1038.47739931446 84 0.15 5.28 8.97 76.12 22.72 44.64 38.71 16.65 1061.88350953149 86 0.15 5.38 8.31 79.42 22.02 46.93 36.7 16.38 1091.8407739278 88 0.15 5.24 8.5 77.38 20.58 48.89 37.74 13.37 1118.15073244554 90 0.15 5.88 10.33 76.73 23.17 45.06 37.2 17.74 1144.86162554337 92 0.15 5.27 9.04 77.72 21.45 47.31 37.46 15.23 1172.85120842733 94 0.15 5.34 9.19 78.03 20.44 48.05 38.68 13.27 1200.38403249822 96 0.15 5.38 9.36 78.08 22.82 45.37 36.93 17.7 1226.57720256158 98 0.15 5.33 8.49 76.65 24.08 44.41 35.61 19.98 1256.5164186396 100 0.13 5.34 9.52 75.09 23.42 45.95 35.16 18.89 1278.72267735565 102 0.14 5.22 9.21 78.44 22.91 45.47 37.19 17.33 1300.92405046733 104 0.14 5.03 9 78.22 24.09 43.31 37.36 19.33 1320.72022592238 106 0.14 5.19 9.57 77.33 21.45 46.22 39.02 14.76 1351.3720267996 108 0.14 5.1 9.59 75.47 21.92 45.64 39.47 14.89 1386.68760141425 110 0.14 4.92 9.13 74.87 22.22 44.76 39.56 15.67 1419.56492317861 112 0.14 5.1 9.12 75.68 21.96 46.62 37.7 15.68 1458.91975952316 114 0.14 5.02 8.82 78.04 23.33 45.09 37.32 17.59 1492.50785856515 116 0.15 4.95 8.98 76.04 23.93 44.35 36.83 18.82 1532.3189878103 118 0.15 4.9 9.22 77.68 23.19 46.29 35.48 18.23 1572.09557659723 120 0.14 5.04 8.77 76.67 22 45.91 37.96 16.13 1602.60130326812 122 0.13 4.94 9.42 77.62 23.47 44.68 37.11 18.21 1635.64185629862 124 0.15 5.03 9.04 77.52 22.38 44.77 38.67 16.56 1668.24078154258 126 0.17 4.96 8.84 75.45 23.3 44.09 37.37 18.54 1696.88611129585 128 0.14 5.03 9.42 77.53 22.99 44.61 37.77 17.62 1731.13957861465 130 0.13 4.98 8.9 76.21 23.56 44.22 37.41 18.37 1765.82927832199 132 0.11 5.04 9.79 77.13 26.5 42.33 36.62 21.06 1805.66024770852 134 0.11 4.97 9.31 76.68 24.48 42.98 37.54 19.48 1844.96799448032 136 0.11 4.94 9.3 75.78 23.7 44.42 36.57 19.01 1884.70494299327 138 0.11 4.94 9.57 77.14 23.73 43.57 37.7 18.73 1926.76985811644 140 0.11 5.11 9.74 75.65 23.88 43.12 38.35 18.53 1964.89386601347 142 0.12 5.1 9.96 75.8 24.05 44.65 36 19.35 2002.45121343643 144 0.12 5.08 10.06 77.11 23.58 42.71 38.89 18.41 2035.62349540428 146 0.12 4.96 9.89 77.14 23.58 43.63 37.19 19.18 2070.14165786614 148 0.16 5.09 9.56 75.91 20.92 47.02 38.88 14.1 2099.06899359129 150 0.1 4.92 9.71 76.21 22.3 45.85 37.99 16.16 2138.3456141596 152 0.11 4.91 10.15 73.21 23.06 45.67 36.48 17.85 2170.33389120752 154 0.11 4.87 9.39 76.11 24.17 43.39 37.67 18.94 2207.35731555999 156 0.11 4.86 9.56 75.54 23.53 43.86 38.18 17.96 2241.60640064831 158 0.11 4.93 10.23 76.01 24.35 42.65 38.32 19.03 2272.52096908752 160 0.13 5 8.91 76.19 23.34 43.33 39.41 17.25 2310.1397242619 162 0.13 5 10.31 77.16 23.19 43.76 38.58 17.66 2339.51805594851 164 0.13 4.92 9.47 75.74 25.06 43.83 36.02 20.15 2369.24488217116 166 0.13 5.1 8.96 74.53 22.56 44.32 38.88 16.8 2404.64507265307 168 0.14 4.87 9.82 73.84 24.33 41.89 38.8 19.32 2432.75052671762 170 0.14 4.85 9.96 75.27 26.07 40.53 37.38 22.09 2463.05968390099 172 0.15 5.07 9.5 76.43 24.15 41.97 38.47 19.56 2490.5231554246 174 0.13 5.01 9.11 76.59 23.75 42.51 39.84 17.66 2526.65942961228 176 0.12 5.04 10.03 76.21 23.5 43.33 39.39 17.28 2571.4582496907 178 0.13 4.98 9.84 74.44 24.69 42.24 36.8 20.96 2607.86194288238 180 0.12 5.09 8.89 76.56 35.12 38.68 43.76 17.56 2645.77892665901 182 0.13 4.97 8.84 77.07 23.61 43.72 37.46 18.83 2680.73705095961 184 0.12 4.97 9.31 74.87 24.36 42.78 36.8 20.43 2717.45877233387 186 0.13 4.94 8.76 76.37 50.22 40.81 43.33 15.86 2751.97620139168 188 0.13 4.95 9.13 77.43 23.34 44.53 37.48 17.99 2780.82965449782 190 0.14 5.14 9.23 77.8 26.49 39.92 40.79 19.28 2818.61451917268 192 0.14 4.93 9.13 76.26 25.52 43.62 35.68 20.7 2852.17948098653 194 0.13 5.09 9.63 76.57 24.35 44.28 35.77 19.95 2887.04055792356 196 0.13 5.11 9.18 76.4 24.03 44.07 36.74 19.18 2931.98302540079 198 0.13 5.05 9.96 76.49 23.42 42.69 39.25 18.06 2971.78273456396 200 0.11 4.99 8.88 76.39 23.72 43.32 38.3 18.39 3007.95988203208 202 0.12 4.91 8.73 76.11 23 45.2 37.05 17.75 3050.38198909861 204 0.13 5.05 9.21 76.18 23.01 44.96 38.5 16.54 3088.76799782257 206 0.14 5.01 8.84 76.37 24.12 43.06 37.4 19.54 3128.97405258019 208 0.13 5.11 9.27 75.59 25.38 42.95 35.88 21.17 3167.58588053822 210 0.12 5.03 8.13 77.92 39.02 40.17 41.98 17.86 3197.15520768475 212 0.14 5 7.98 76.62 24.72 43.51 36.73 19.76 3231.66622876633 214 0.12 5 7.7 77.85 25.03 42.83 36.58 20.58 3267.40158938255 216 0.12 4.95 7.67 76.34 22.36 45.27 38.82 15.91 3331.51750482614 218 0.12 5.09 7.93 76.18 24.01 40.89 41.49 17.62 3386.26045545335 220 0.11 5.1 10.38 75.93 22.88 45.09 37.82 17.1 3444.30157873862 222 0.12 5.16 10.42 74.64 24.51 41.12 42.76 16.11 3505.41416507922 224 0.12 5.15 10.49 74.69 21.34 47.57 37.9 14.53 3567.43141064749 226 0.12 5.19 10.35 74.21 23.2 45.91 36.64 17.44 3619.6832721105 228 0.13 5.07 10.01 75.26 24.11 43.47 36.6 19.93 3667.40822506297 230 0.12 4.97 10.06 74.29 24.21 44.39 36.45 19.16 3716.94281408555 232 0.12 4.94 10.16 74.27 23.72 44.63 36.92 18.45 3782.58019525149 234 0.12 5.17 9.92 75.35 22.49 45.71 37.68 16.62 3841.92902595806 236 0.12 5 10.33 74.96 21.5 45.87 39.35 14.78 3895.78284139882 238 0.13 4.86 9.46 74.64 23.97 43.55 38.08 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