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  • 11
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    PANGAEA
    In:  Supplement to: Meyer, Vera D; Hefter, Jens; Köhler, Peter; Tiedemann, Ralf; Gersonde, Rainer; Wacker, Lukas; Mollenhauer, Gesine (2019): Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming. Environmental Research Letters, 14(8), 085003, https://doi.org/10.1088/1748-9326/ab2653
    Publication Date: 2023-01-13
    Description: The dataset comprises contents, mass-accumulation rates and compound-specific radiocarbon data of several terrigenous biomarkers in sediment cores from the Northwest Pacific (core SO201-2-12KL) and the Bering Sea (cores SO201-2-114KL, SO202/1_18-6 and SO202/1_18-3). The dataset includes contents and mass accumulation rates of high molecular weight n-alkanoic acids, high molecular weight n-alkanes and branched glycerol dialkyl glycerol tetraethers. Moreover, contents and fractional abundances of homohopane isomers are given. Contents are calculated relative to total organic carbon contents and to the dry weight of the sediment. The dataset also contains Paq values and the carbon preference indices of n-alkanoic acids and n-alkanes. Compound-specific radiocarbon data have been obtained from high molecular weight n-alkanoic acids (n-C26:0 alkanoic acid) and high molecular weight n-alkanes (n-C23, n-C27 and n-C29 alkanes). The F14C has been corrected for procedural blanks associated with the isolation of the biomarkers. The data compilation contains the measured (AMS-results) as well as the blank-corrected F14C values. The 14C-data are reported with the 1sigma uncertainty.
    Type: Dataset
    Format: application/zip, 12 datasets
    Location Call Number Limitation Availability
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  • 12
    Publication Date: 2023-01-13
    Description: The comparison between different climate model simulations of water hosing experiments under glacial conditions points toward diverging responses in Sea Surface Temperature changes (SST) especially in the Southeast Pacific (SEP). This suggests that reconstituting the latitudinal SST gradient in the SEP is a critical parameter for a better understanding of the mechanisms behind the abrupt climatic events since the last glacial period. Here we present, high-resolution records of SST, using planktonic foraminiferal assemblages and alkenone temperature reconstructions and stable oxygen and carbon isotopes from three deep-sea sediment cores along a latitudinal transect off the southern Chilean coast. This allowed us to reconstruct the variations of the latitudinal SST gradient and the Subtropical Front movements in the SEP. The SST results suggest a clear Antarctic timing consistent with the bipolar seesaw control, especially during the late glacial and the deglaciation. Our records do not suggest a complete oceanic heat transfer signal, highlighting the implication of an atmospheric component in the heat transfers between the two hemispheres, controlled by the latitudinal movements of the intertropical convergence zone in the Atlantic and the associated weaker South Pacific westerly split jet. Furthermore, our records indicate variable conditions during the Holocene, and also emphasize the influence of local fresh water inputs from the Patagonian ice sheet and/or precipitation on the SST fresh water input estimates along the Chilean margin (North and South of 49° S) from the onset of the deglaciation until 8 kyr cal. BP.
    Keywords: chilean margin; planktonic foraminifera d18O; Sea surface temperatures during the last 22 kyrs
    Type: Dataset
    Format: application/zip, 10 datasets
    Location Call Number Limitation Availability
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  • 13
    Publication Date: 2023-01-30
    Keywords: CBeu; DATE/TIME; Deviation angle; diol; diol proxy; Mauritania; sediment trap; Temperature; Upwelling; wind; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 5967 data points
    Location Call Number Limitation Availability
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  • 14
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    PANGAEA
    In:  Supplement to: Ceccopieri, Milena; Carreira, Renato S; Wagener, Angela L R; Hefter, Jens; Mollenhauer, Gesine (2018): On the application of alkenone- and GDGT-based temperature proxies in the south-eastern Brazilian continental margin. Organic Geochemistry, 126, 43-56, https://doi.org/10.1016/j.orggeochem.2018.10.009
    Publication Date: 2023-02-07
    Description: The applicability of two organic geochemical proxies (UK'37 based on alkenones and TEXH86 based on glycerol dialkyl glycerol tetraethers) for ocean temperatures was investigated on a regional scale in the SE Brazilian continental margin (Campos Basin) using 53 core-top sediments. In 71% of the samples for UK'37 and 85% for TEXH86, the estimated annual mean sea surface temperature (SST) is comparable to the climatological annual mean data, with deviations within the calibration error. The surface TEXH86 estimates reflects the surface mixed layer, while the depth-integrated (0-200 m) TEXH86 estimates showed better agreement with temperatures at 100-200 mdepth. In addition, the SST-UK'37 results were more consistent (73% of the samples) using a winter calibration rather than an annual mean calibration. This seasonal effect might be ascribed to an increase in the abundance of haptophytes in the region during the winter. Exceptions to these general trends were observed for both proxies as a strong cold bias in reconstructed temperature in a few samples in the southern portion of the studied region, which may be related to (i) a predominant subsurface habitat of Thaumarchaeota combined with enhanced primary production and flux of particles during upwelling and (ii) alkenones being laterally transported from adjacent colder waters. Effects of river input of terrestrially sourced GDGTs on TEXH86 are not evident. Overall, our findings show that UK'37 and TEXH86 are suitable temperature proxies for paleoclimate studies at a regional scale in the SE Brazilian continental margin, but on a local scale the effects of upwelling must be taken in consideration.
    Keywords: A01; A02; A03; A04; A05; A06; A07; A08; A09; A10; A11; A12; Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Alkenone, per unit mass total organic carbon; Alkenone, unsaturation index UK'37; Alkenone per unit sediment mass; B1; B10; B11; B12; B2; B3; B4; B5; B6; B7; B8; B9; BCM; Box corer, modified; Cabo Frio upwelling system; Campos Basin; Campos Basin Environmental Heterogeneity Project (CENPES/Petrobras); Crenarchaeol, fractional abundance; Crenarchaeol isomer, fractional abundance; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Event label; extracted from the World Ocean Atlas 2013 (WOA13); G03; G04; G05; G07; G08; G09; G10; G11; G12; Gyre; H1; H10; H11; H12; H2; H3; H4; H5; H6; H7; HAB_A01; HAB_A02; HAB_A03; HAB_A04; HAB_A05; HAB_A06; HAB_A07; HAB_A08; HAB_A09; HAB_A10; HAB_A11; HAB_A12; HAB_B1; HAB_B10; HAB_B11; HAB_B12; HAB_B2; HAB_B3; HAB_B4; HAB_B5; HAB_B6; HAB_B7; HAB_B8; HAB_B9; HAB_G03; HAB_G04; HAB_G05; HAB_G07; HAB_G08; HAB_G09; HAB_G10; HAB_G11; HAB_G12; HAB_H1; HAB_H10; HAB_H11; HAB_H12; HAB_H2; HAB_H3; HAB_H4; HAB_H5; HAB_H6; HAB_H7; HAB_I02; HAB_I04; HAB_I05; HAB_I06; HAB_I07; HAB_I08; HAB_I09; HAB_I10; HAB_I11; HAB_I12; HAB10; HAB11; HAB13; HAB5; HAB8; HAB9; Habitats; High Performance Liquid Chromatography (HPLC-APCI-MS); I02; I04; I05; I06; I07; I08; I09; I10; I11; I12; Isoprenoid glycerol dialkyl glycerol tetraether, per unit mass total organic carbon; Isoprenoid glycerol dialkyl glycerol tetraether, per unit sediment mass; Miss Emma McCall; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; Sea surface temperature, annual mean; South Atlantic Ocean; surface sediments; Tetraether index of 86 carbon atoms; TEXH86; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance; UK'37; van Veen Grab, modified; VGRABM
    Type: Dataset
    Format: text/tab-separated-values, 745 data points
    Location Call Number Limitation Availability
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  • 15
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    PANGAEA
    In:  Supplement to: Meyer, Vera D; Hefter, Jens; Lohmann, Gerrit; Max, Lars; Tiedemann, Ralf; Mollenhauer, Gesine (2017): Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20000 years. Climate of the Past, 13(4), 359-377, https://doi.org/10.5194/cp-13-359-2017
    Publication Date: 2023-03-16
    Description: Little is known about the climate evolution on the Kamchatka Peninsula during the last glacial?interglacial transition as existing climate records do not reach beyond 12 ka BP. In this study, a summer temperature record for the past 20 kyr is presented. Branched glycerol dialkyl glycerol tetraethers, terrigenous biomarkers suitable for continental air temperature reconstructions, were analyzed in a sediment core from the western continental margin off Kamchatka in the marginal northwest Pacific (NW Pacific). The record suggests that summer temperatures on Kamchatka during the Last Glacial Maximum (LGM) equaled modern temperatures. We suggest that strong southerly winds associated with a pronounced North Pacific High pressure system over the subarctic NW Pacific accounted for the warm conditions. A comparison with an Earth system model reveals discrepancies between model and proxy-based reconstructions for the LGM temperature and atmospheric circulation in the NW Pacific realm. The deglacial temperature development is characterized by abrupt millennial-scale temperature oscillations. The Bølling?Allerød warm phase and the Younger Dryas cold spell are pronounced events, suggesting a connection to North Atlantic climate variability.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 16
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    PANGAEA
    In:  Supplement to: Meyer, Vera D; Max, Lars; Hefter, Jens; Tiedemann, Ralf; Mollenhauer, Gesine (2016): Glacial-to-Holocene evolution of sea surface temperature and surface circulation in the subarctic northwest Pacific and the Western Bering Sea. Paleoceanography, 31, 12 pp, https://doi.org/10.1002/2015PA002877
    Publication Date: 2023-03-16
    Description: It has been proposed that North Pacific sea surface temperature (SST) evolution was intimately linked to North Atlantic climate oscillations during the last glacial-interglacial transition. However, during the early deglaciation and the Last Glacial Maximum, the SST development in the subarctic northwest Pacific and the Bering Sea is poorly constrained as most existing deglacial SST records are based on alkenone paleothermometry, which is limited prior to 15 ka B.P. in the subarctic North Pacific realm. By applying the TEXL86 temperature proxy we obtain glacial-Holocene-SST records for the marginal northwest Pacific and the Western Bering Sea. Our TEXL86-based records and existing alkenone data suggest that during the past 15.5 ka, SSTs in the northwest Pacific and the Western Bering Sea closely followed millennial-scale climate fluctuations known from Greenland ice cores, indicating rapid atmospheric teleconnections with abrupt climate changes in the North Atlantic. Our SST reconstructions indicate that in the Western Bering Sea SSTs drop significantly during Heinrich Stadial 1 (HS1), similar to the known North Atlantic climate history. In contrast, progressively rising SST in the northwest Pacific is different to the North Atlantic climate development during HS1. Similarities between the northwest Pacific SST and climate records from the Gulf of Alaska point to a stronger influence of Alaskan Stream waters connecting the eastern and western basin of the North Pacific during this time. During the Holocene, dissimilar climate trends point to reduced influence of the Alaskan Stream in the northwest Pacific.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 17
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
    Location Call Number Limitation Availability
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  • 18
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, carbon dioxide, aquatic
    Type: Dataset
    Format: text/tab-separated-values, 198 data points
    Location Call Number Limitation Availability
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  • 19
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
    Location Call Number Limitation Availability
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  • 20
    Publication Date: 2023-05-12
    Keywords: Alkenone per cell Emiliania huxleyi; Europe, Norway; MESO; Mesocosm experiment; ORDINAL NUMBER; Pressurized liquid extraction; Raunefjord
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
    Location Call Number Limitation Availability
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