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  • 1
    Publication Date: 2021-02-16
    Description: Abrupt climate changes during the last glacial period have been detected in a global array of palaeoclimate records, but our understanding of their absolute timing and regional synchrony is incomplete. Our compilation of 63 published, independently dated speleothem records shows that abrupt warmings in Greenland were associated with synchronous climate changes across the Asian Monsoon, South American Monsoon, and European-Mediterranean regions that occurred within decades. Together with the demonstration of bipolar synchrony in atmospheric response, this provides independent evidence of synchronous high-latitude–to-tropical coupling of climate changes during these abrupt warmings. Our results provide a globally coherent framework with which to validate model simulations of abrupt climate change and to constrain ice-core chronologies.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 2
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    Elsevier
    In:  EPIC3Palaeogeography Palaeoclimatology Palaeoecology, Elsevier, 632, pp. 111863-111863, ISSN: 0031-0182
    Publication Date: 2024-04-22
    Description: Winter climate variations in midlatitude regions have far-reaching effects on both natural and human systems worldwide. However, most climate reconstructions focus on either annual or summer climate conditions. Here we present a stalagmite stable isotope record from Urşilor Cave (Romania) where the δ18O values are controlled by winter temperature. Because of its East-Central Europe (ECE) location, the cave site is well suited to capture variations in precipitation and temperature in response to changes in the North Atlantic region. Present day precipitation and temperature in this region are controlled by two teleconnection patterns, the Arctic Oscillation (AO) and the East Atlantic (EA). By analyzing composite maps for four different scenarios of AO and EA phase, we suggest that between 5.6 and 5.2 ka the positive phases of AO and EA became increasingly dominant. This shift led to generally warmer winters in northern Europe, but drier conditions in southern Europe and the Levant. Considering the compound effect of AO and EA on the hydroclimate of ECE, our study highlights the importance of examining the combined impact of teleconnection patterns on climate proxies influenced by various forcing mechanisms.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 3
    Publication Date: 2024-03-25
    Description: In this study, the dead carbon fraction (DCF) variations in stalagmite M1-5 from Socotra Island in the western Arabian Sea were investigated through a new set of high-precision U-series and radiocarbon (14C) dates. The data reveal an extreme case of very high and also climate dependent DCF values. For M1-5 an average DCF of 56.2 ± 3.4 % is observed between 27 and 18 kyr BP. Such high DCF values indicate a high influence of aged soil organic matter (SOM) and nearly completely closed system carbonate dissolution conditions. Towards the end of the last glacial period decreasing Mg/Ca ratios suggest an increase in precipitation which caused a marked change in the soil carbon cycling as indicated by sharply decreasing DCF. This is in contrast to the relation of soil infiltration and reservoir age observed in stalagmites from temperate zones. For Socotra Island, which is influenced by the East African-Indian monsoon, we propose that more humid conditions and enhanced net-infiltration after the LGM led to denser vegetation and thus lowered the DCF by increased 14CO2 input into the soil zone. The onset of the Younger Dryas (YD) is represented in the record by the end of DCF decrease with a sudden change to much higher and extremely variable reservoir ages. Our study highlights the dramatic variability of soil carbon cycling processes and vegetation feedback on Socotra Island manifested in stalagmite reservoir ages on both long-term trends and sub-centennial timescales, thus providing evidence for climate influence on stalagmite radiocarbon. This is of particular importance for studies focussing on 14C calibration and atmospheric reconstruction through stalagmites which relies on largely climate independent soil carbon cycling above the cave.
    Keywords: Dead Carbon Fraction; radiocarbon; Socotra; speleothem; U-series
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Shumilovskikh, Lyudmila S; Fleitmann, Dominik; Nowaczyk, Norbert R; Behling, Hermann; Marret, Fabienne; Wegwerth, Antje; Arz, Helge Wolfgang (2014): Orbital- and millennial-scale environmental changes between 64 and 20 ka BP recorded in Black Sea sediments. Climate of the Past, 10(3), 939-954, https://doi.org/10.5194/cp-10-939-2014
    Publication Date: 2024-03-25
    Description: High-resolution pollen and dinoflagellate cyst records from sediment core M72/5-25-GC1 were used to reconstruct vegetation dynamics in northern Anatolia and surface conditions of the Black Sea between 64 and 20 ka BP. During this period, the dominance of Artemisia in the pollen record indicates a steppe landscape and arid climate conditions. However, the concomitant presence of temperate arboreal pollen suggests the existence of glacial refugia in northern Anatolia. Long-term glacial vegetation dynamics reveal two major arid phases ~64-55 and 40-32 ka BP, and two major humid phases ~54-45 and 28-20 ka BP, correlating with higher and lower summer insolation, respectively. Dansgaard-Oeschger (D-O) cycles are clearly indicated by the 25-GC1 pollen record. Greenland interstadials are characterized by a marked increase in temperate tree pollen, indicating a spread of forests due to warm/wet conditions in northern Anatolia, whereas Greenland stadials reveal cold and arid conditions as indicated by spread of xerophytic biomes. There is evidence for a phase lag of ~500 to 1500 yr between initial warming and forest expansion, possibly due to successive changes in atmospheric circulation in the North Atlantic sector. The dominance of Pyxidinopsis psilata and Spiniferites cruciformis in the dinocyst record indicates brackish Black Sea conditions during the entire glacial period. The decrease of marine indicators (marine dinocysts, acritarchs) at ~54 ka BP and increase of freshwater algae (Pediastrum, Botryococcus) from 32 to 25 ka BP reveals freshening of the Black Sea surface water. This freshening is possibly related to humid phases in the region, to connection between Caspian Sea and Black Sea, to seasonal freshening by floating ice, and/or to closer position of river mouths due to low sea level. In the southern Black Sea, Greenland interstadials are clearly indicated by high dinocyst concentrations and calcium carbonate content, as a result of an increase in primary productivity. Heinrich events show a similar impact on the environment in the northern Anatolia/Black Sea region as Greenland stadials.
    Keywords: 25-GC1; Abies; Acer; AGE; Alisma-type; Alnus; Apiaceae; Artemisia; Asteraceae; Ballota-type; Betula; Bistorta-type; Bitectatodinium tepikiense; Black Sea; Botryococcus; Brassicaceae; Buxus; Campanula trachelium-type; Cannabaceae; Carpinus betulus; Carya; Caryophyllaceae; Caspidinium rugosum; Castanea; Cedrus; Celtis; Centaurea alpina-type; Centaurea cyanus; Centaurea jacea-type; Cerealia-type; Chenopodiaceae; Cirsium; Cistus salvifolius; Coniferae; Cornus mas-type; Corylus; Cotinus coggygria; Counting, palynology; Cymatiosphaera; Cynoglossum; Cyperaceae; DEPTH, sediment/rock; Dinoflagellate cyst indeterminata; Dinoflagellate cyst reworked; Ephedra distachya-type; Ephedra fragilis-type; Ericaceae; Fabaceae; Fagus; Filipendula; Frangula alnus; Fraxinus angustifolia var. oxycarpa; Fraxinus excelsior-type; Galeopsis-type; GC; Gentiana pneumonanthe-type; Glomus; Gravity corer; Haloxylon; Hedera helix-type; Hedysarum hedysaroides; Helianthemum nummularium group; Helianthemum oelandicum-type; Helleborus foetidus; Hippophae; Ilex; Indeterminata; Jasione montana-type; Juglans; Juniperus; Knautia; Liguliflorae; Liliaceae; Lingulodinium machaerophorum; Linum; Liquidambar; Lycopodium spores counted; Lycopodium spores per tablet; Lycopodium tablets; M72/5; M72/5_628-1; Matricaria-type; Mentha-type; Meteor (1986); Micrhystridium; Multiplicisphaeridium; Muscari neglectum-type; Myrica; Olea; Operculodinium centrocarpum; Ornithogalum umbellatum-type; Ostrya-type; Papaver rhoeas group; Pediastrum; Phillyrea; Picea; Pinus; Pinus diploxylon-type; Pinus haploxylon-type; Pistacia; Plantago lanceolata-type; Plantago major/media-type; Plantago maritima-type; Platanus orientalis; Plumbaginaceae; Poaceae; Pollen, reworked; Polygonum aviculare-type; Potamogeton natans-type; Potentilla-type; Prunus-type; Pterocarya; Pulmonaria-type; Pyxidinopsis psilata; Quercus cerris-type; Quercus ilex-type; Quercus robur-type; Ranunculus acris-type; Rhamnus-type; Rheum; Rhinanthus-type; Rubiaceae; Rumex; Salix; Sambucus ebulus; Sanguisorba minor-type; Saussurea-type; Saxifraga aizoides-type; Saxifraga cuneifolia-type; Saxifraga stellaris-type; Scabiosa argentea; Scrophulariaceae; Senecio-type; Sorbus group; Sparganium-type; Spiniferites bentori; Spiniferites cruciformis; Spiniferites pachydermus; Spiniferites spp.; Symphytum; Tamarix; Taxus; Tectatodinium pellitum; Thalictrum; Tilia; Tribulus terrestris; Tsuga; Tuberculodinium vancampoae; Ulmus/Zelkova; Valeriana saxatilis-type; Varia; Verbena officinalis; Viburnum lantana; Vitis; Xanthium spinosum-type; Zygnemataceae
    Type: Dataset
    Format: text/tab-separated-values, 24450 data points
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  • 5
    Publication Date: 2024-03-25
    Keywords: GIK17041-2; KAL; Kasten corer; North Al-Wajh Deeps; ROTES MEER; SO121; SO121_93; Sonne
    Type: Dataset
    Format: unknown
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  • 6
    Publication Date: 2024-03-25
    Keywords: GIK17042-2; KAL; Kasten corer; North Al-Wajh Deeps; ROTES MEER; SO121; SO121_95; Sonne
    Type: Dataset
    Format: unknown
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  • 7
    Publication Date: 2024-03-25
    Keywords: AGE; HAND; Milandre_Cave; Sampling by hand; Switzerland; Temperature, annual mean; Temperature, annual mean, uncertainty
    Type: Dataset
    Format: text/tab-separated-values, 1596 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-03-25
    Description: In this study, the dead carbon fraction (DCF) variations in stalagmite M1-5 from Socotra Island in the western Arabian Sea were investigated through a new set of high-precision U-series and radiocarbon (14C) dates. The data reveal an extreme case of very high and also climate dependent DCF values. For M1-5 an average DCF of 56.2 ± 3.4 % is observed between 27 and 18 kyr BP. Such high DCF values indicate a high influence of aged soil organic matter (SOM) and nearly completely closed system carbonate dissolution conditions. Towards the end of the last glacial period decreasing Mg/Ca ratios suggest an increase in precipitation which caused a marked change in the soil carbon cycling as indicated by sharply decreasing DCF. This is in contrast to the relation of soil infiltration and reservoir age observed in stalagmites from temperate zones. For Socotra Island, which is influenced by the East African-Indian monsoon, we propose that more humid conditions and enhanced net-infiltration after the LGM led to denser vegetation and thus lowered the DCF by increased 14CO2 input into the soil zone. The onset of the Younger Dryas (YD) is represented in the record by the end of DCF decrease with a sudden change to much higher and extremely variable reservoir ages. Our study highlights the dramatic variability of soil carbon cycling processes and vegetation feedback on Socotra Island manifested in stalagmite reservoir ages on both long-term trends and sub-centennial timescales, thus providing evidence for climate influence on stalagmite radiocarbon. This is of particular importance for studies focussing on 14C calibration and atmospheric reconstruction through stalagmites which relies on largely climate independent soil carbon cycling above the cave.
    Keywords: Accelerator mass spectrometry (AMS); AGE; Age, AMS 14C conventional; Age, dated; Age, standard deviation; Age, Uranium-Thorium; Carbon-14, modern; Carbon-14, modern, atmosphere; Carbon-14, modern, atmosphere, standard deviation; Carbon-14, modern, error; Carbon-14, modern, initial; Carbon-14, modern, initial, standard deviation; Carbon-14, modern, standard deviation; Dead carbon fraction; Dead Carbon Fraction; Dead carbon fraction, standard deviation; DISTANCE; Moomi_Cave_2002; Moomi_Cave_M1-5; radiocarbon; Sample code/label; Socotra; Socotra Island, Arabian Sea; speleothem; Speleothem sample; SPS; U-series
    Type: Dataset
    Format: text/tab-separated-values, 1014 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-03-25
    Keywords: GIK17032-1; KAL; Kasten corer; Kebrit Deep; ROTES MEER; SO121; SO121_48; Sonne
    Type: Dataset
    Format: unknown
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-03-25
    Keywords: Age; AGE; Braarudosphaera spp.; Coccoliths, warm; DEPTH, sediment/rock; Eastern Mediterranean Sea; Emiliania huxleyi; Florisphaera profunda; Helicosphaera spp.; MEDECOS_II_M2; MUC; MultiCorer
    Type: Dataset
    Format: text/tab-separated-values, 558 data points
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