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  • 1
    Publikationsdatum: 2023-11-24
    Beschreibung: Elemental scans, organic geochemistry and stable isotope analysis is presented here from a stomach-oil deposit collected at Lake Untersee in central Dronning Maud Land (DML). Deposit WMM7 (sometimes called Antarctic mumiyo) was collected at -71.367 degN, 13.317 degE during the GeoMaud expedition (1995/1996), from the Untersee Oasis, Dronning Maud Land. The aim of the analysis is to investigate snow petrel diet during the Last Glacial stage (22-29 ka) and in turn to infer changing sea-ice conditions in the South Atlantic sector of the Southern Ocean (McClymont et al., Climate of the Past Discussions, submitted). The data include results from non-destructive XRF scanning (ITRAX core scanner, National Oceanography Centre, Southampton, U.K.), fatty acid distributions and fatty acid stable isotope ratios (Department of Geography, Durham University, Durham, U.K.) and bulk stable carbon and nitrogen isotope ratios (Department of Earth Sciences, Durham University, Durham, U.K.). The age-depth model is constrained by 6 new bulk radiocarbon measurements (CologneAMS, Cologne, Germany).
    Schlagwort(e): Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Biomarker; fatty acid; Last Glacial; mumiyo; Sea ice; Stable isotope; XRF
    Materialart: Dataset
    Format: application/zip, 5 datasets
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Watcham, Emma P; Bentley, Michael J; Hodgson, Dominic A; Roberts, Stephen J; Fretwell, Peter; Lloyd, Jerry M; Larter, Robert D; Whitehouse, Pippa L; Leng, Melanie J; Monien, Patrick; Moreton, Steven Grahame (2011): A new Holocene relative sea level curve for the South Shetland Islands, Antarctica. Quaternary Science Reviews, 30(21-22), 3152-3170, https://doi.org/10.1016/j.quascirev.2011.07.021
    Publikationsdatum: 2023-11-04
    Beschreibung: Precise relative sea level (RSL) data are important for inferring regional ice sheet histories, as well as helping to validate numerical models of ice sheet evolution and glacial isostatic adjustment. Here we develop a new RSL curve for Fildes Peninsula, South Shetland Islands (SSIs), a sub-Antarctic archipelago peripheral to the northern Antarctic Peninsula ice sheet, by integrating sedimentary evidence from isolation basins with geomorphological evidence from raised beaches. This combined approach yields not only a Holocene RSL curve, but also the spatial pattern of how RSL change varied across the archipelago. The curve shows a mid-Holocene RSL highstand on Fildes Peninsula at 15.5 m above mean sea level between 8000 and 7000 cal a BP. Subsequently RSL gradually fell as a consequence of isostatic uplift in response to regional deglaciation. We propose that isostatic uplift occurred at a non-steady rate, with a temporary pause in ice retreat ca. 7200 cal a BP, leading to a short-lived RSL rise of ~1 m and forming a second peak to the mid-Holocene highstand. Two independent approaches were taken to constrain the long-term tectonic uplift rate of the SSIs at 0.22-0.48 m/ka, placing the tectonic contribution to the reconstructed RSL highstand between 1.4 and 2.9 m. Finally, we make comparisons to predictions from three global sea level models.
    Schlagwort(e): Age, 14C calibrated, CALIB (Stuiver & Reimer, 1993); Age, 14C milieu/reservoir corrected (Milliken et al., 2009); Age, AMS 14C conventional; Age, dated; Age, dated material; Age, dated standard deviation; Ardley_lake; Belen_lake; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Comment of event; Core; CORE; Event label; Fildes Peninsula, King George Island; Gaoshan_lake; Laboratory; Laguna_Tern, Lake_Albatross; Lake_Shanhaicuan; Latitude of event; Long_lake; Longitude of event; Ozero_Dlinnoye; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Probability; Sample ID; SPP1158; Yanou_lake; Yue_Ya_Hu, Laguna_Ripamonti; δ13C
    Materialart: Dataset
    Format: text/tab-separated-values, 928 data points
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  • 3
    Publikationsdatum: 2023-11-24
    Beschreibung: XRF analysis of stomach-oil deposit WMM7.
    Schlagwort(e): AGE; Aluminium; Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Arsenic; Barium; Bromine; Calcium; Cerium; Chlorine; Chromium; Copper; DEPTH, sediment/rock; Gallium; GeoMaud95/96; Iron; Last Glacial; Lead; Manganese; MULT; Multiple investigations; mumiyo; Nickel; Phosphorus; Potassium; Rubidium; Sampling on land; Sea ice; Silicon; Strontium; Sulfur; Titanium; Unterseeoase; Vanadium; WMM-7; X-ray fluorescence ITRAX core scanner; XRF; Zinc; Zirconium
    Materialart: Dataset
    Format: text/tab-separated-values, 18960 data points
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  • 4
    Publikationsdatum: 2023-11-24
    Beschreibung: Total nitrogen %, total organic carbon % and bulk stable isotope ratios of carbon and nitrogen for stomach-oil deposit WMM7. Standard deviations reported for replicate analyses.
    Schlagwort(e): AGE; Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Biomarker; Carbon, organic, total; Carbon/Nitrogen ratio; DEPTH, sediment/rock; Element analyser isotope ratio mass spectrometer (EA-IRMS); GeoMaud95/96; Last Glacial; MULT; Multiple investigations; mumiyo; Nitrogen, total; Sampling on land; Sea ice; Stable isotope; Unterseeoase; WMM-7; δ13C; δ13C, standard deviation; δ15N; δ15N, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 5
    Publikationsdatum: 2023-11-24
    Beschreibung: Fatty acid and selected pigment distributions from stomach-oil deposit WMM7. Pigments are reported according to the absorbance at 4 key wavelengths (e.g. P410 = absorbance at 410 nm). Absorbances are reported normalised to extracted mass of stomach-oil deposit (abs g-1) and normalised to total organic carbon content (abs gTOC-1).
    Schlagwort(e): AGE; Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Biomarker; cis-9-Octadecenoic acid of total fatty acids (IUPAC: Octadec-9-enoic acid); DEPTH, sediment/rock; fatty acid; Gas chromatography - Mass spectrometry (GC-MS); GeoMaud95/96; Hexadecanoic acid of total fatty acids; Hexadecenoic acid of total fatty acids; Last Glacial; MULT; Multiple investigations; mumiyo; Octadecanoic acid of total fatty acids; Pigments, absorbance at 410 nm, per unit mass total organic carbon; Pigments, absorbance at 410 nm per unit mass; Pigments, absorbance at 435 nm, per unit mass total organic carbon; Pigments, absorbance at 435 nm per unit mass; Pigments, absorbance at 660 nm, per unit mass total organic carbon; Pigments, absorbance at 660 nm per unit mass; Pigments, absorbance at 665 nm, per unit mass total organic carbon; Pigments, absorbance at 665 nm per unit mass; Sampling on land; Sea ice; Tetradecanoic acid of total fatty acids; Unterseeoase; UV-visible spectrophotometer; WMM-7
    Materialart: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 6
    Publikationsdatum: 2023-11-24
    Beschreibung: Fatty acid stable carbon isotope ratios from stomach-oil deposit WMM7. Standard deviations reported for duplicate measurements.
    Schlagwort(e): AGE; Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Biomarker; cis-9-Octadecenoic acid, δ13C; cis-9-Octadecenoic acid, δ13C, standard deviation; DEPTH, sediment/rock; fatty acid; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); GeoMaud95/96; Hexadecanoic acid, δ13C; Hexadecanoic acid, δ13C, standard deviation; Last Glacial; MULT; Multiple investigations; mumiyo; Octadecanoic acid, δ13C; Octadecanoic acid, δ13C, standard deviation; Sampling on land; Sea ice; Stable isotope; Tetradecanoic acid, δ13C; Tetradecanoic acid, δ13C, standard deviation; Unterseeoase; WMM-7
    Materialart: Dataset
    Format: text/tab-separated-values, 96 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-04-20
    Beschreibung: High-resolution palaeotopographic and -bathymetric models of the Southern Ocean and the Antarctic continent facilitate detailed investigation of past ice sheet and ocean circulation development from land to sea, which is essential for robust reconstructions of the paleoclimate, palaeocryosphere, and palaeoceanography. These important boundary conditions have been newly reconstructed based on all available geophysical and geological data and merged together to form complete grids of the Southern Ocean and Antarctica. For detailed information on the reconstructions, please refer to Paxman et al. (2019) and Hochmuth et al. (2020) for the palaeotopography and the palaeobathymetry, respectively. For further information on the merging process, please see the attached readme document. We present a compilation of the merged palaeotopography and palaeobathymetry for five key time slices in the Cenozoic development of the Antarctic continent and the Southern Ocean: (i) Eocene/Oligocene Boundary (34 Ma), (ii) Oligocene/Miocene Transition (23 Ma), (iii) middle Miocene (14 Ma), (iv) early Pliocene (5 Ma), and (v) Pliocene/Pleistocene Boundary (2.6 Ma). Note: The primary authors of the original publications, G. Paxman and K. Hochmuth are equally contributing joint first authors of this dataset compilation.
    Schlagwort(e): Antarctica; Binary Object; Binary Object (File Size); Binary Object (Media Type); Eocene/Oligocene Boundary; Miocene; palaeobathymetry; palaeotopography; Pleistocene; Pliocene; Southern Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 8
    Publikationsdatum: 2024-04-29
    Beschreibung: Age determination of stomach-oil deposit WMM7. Radiocarbon ages calibrated to calendar ages using MARINE20 (Heaton et al., 2020) using two scenarios: using Holocene deltaR of 670 ± 50 yr (Björck et al. 1991) or using a simulated sea ice deltaR of 2470 ± 50 yr (Heaton et al., 2020). COL3022 was previously published (Berg et al., 2019).
    Schlagwort(e): Age, 14C calibrated, MARINE20 (Heaton et al., 2020); Age, dated; Age, dated standard deviation; Antarctica; ANTarctic Sea Ice Evolution from a novel biological archive; ANTSIE; Calendar age, maximum/old; Calendar age, median; Calendar age, minimum/young; DEPTH, sediment/rock; GeoMaud95/96; Laboratory code/label; Last Glacial; MULT; Multiple investigations; mumiyo; Sampling on land; Sea ice; Stable isotope; Unterseeoase; WMM-7
    Materialart: Dataset
    Format: text/tab-separated-values, 63 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2020-07-02
    Beschreibung: The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary basins. The extent, geology, and basal topography of these sedimentary basins are important boundary conditions governing the dynamics of the overlying ice sheet. This is particularly pertinent for basins close to the grounding line wherein the EAIS is grounded below sea level and therefore potentially vulnerable to rapid retreat. Here we analyze newly acquired airborne geophysical data over the Pensacola‐Pole Basin (PPB), a previously unexplored sector of the EAIS. Using a combination of gravity and magnetic and ice‐penetrating radar data, we present the first detailed subglacial sedimentary basin model for the PPB. Radar data reveal that the PPB is defined by a topographic depression situated ~500 m below sea level. Gravity and magnetic depth‐to‐source modeling indicate that the southern part of the basin is underlain by a sedimentary succession 2–3 km thick. This is interpreted as an equivalent of the Beacon Supergroup and associated Ferrar dolerites that are exposed along the margin of East Antarctica. However, we find that similar rocks appear to be largely absent from the northern part of the basin, close to the present‐day grounding line. In addition, the eastern margin of the basin is characterized by a major geological boundary and a system of overdeepened subglacial troughs. We suggest that these characteristics of the basin may reflect the behavior of past ice sheets and/or exert an influence on the present‐day dynamics of the overlying EAIS.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 10
    Publikationsdatum: 2020-08-30
    Beschreibung: The Antarctic continent and its surrounding Southern Ocean are a key component of our planet’s climate system. Since the Eocene/Oligocene Boundary (34 Ma) the Antarctic region has undergone tremendous topographical change on the continent and in the oceanic realm. The massive erosion on the continent by the Antarctic ice sheets and the resulting glacial deposition within the Southern Ocean have shaped our modern maps of the Southern hemisphere. Detailed, high-resolution reconstructions of the palaeotopography and palaeobathymetry shed light on crucial periods in the development of the Antarctic ice sheets as well as the Southern Ocean. This includes e.g. the establishment of the modern circum-polar current system, the pathways of modern and ancient glacial systems as well as the role of the continental shelves in ice sheet stability. Most recent reconstructions of the paleotopography (Paxman et al. 2019) and paleobathymetry (Hochmuth et al. 2020) used all available geophysical as well as geological and borehole data to produce high-resolution maps (0.1 deg) of key time slices of the Southern Ocean evolution. The combined palaeobathymetry and palaeotopography allows seamless land-to-ocean studies including analysis of ice sheet behaviour and erosion and associated depositional cycles. The five time slices presented span from the onset of continental glaciation in Antarctica (34 Ma) to the warmer climates of the Miocene and early Pliocene to the manifestation of modern glacial condition at the Pliocene/Pleistocene Boundary.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
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