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  • 11
    Publication Date: 2023-06-27
    Keywords: AGE; Amphibole/standard ratio; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic total/Sulfur, total, ratio; Density; DEPTH, sediment/rock; Feldspar/standard ratio; Lake Fryxell, East Antarctica; Lz1021; Magnetic susceptibility, volume; Nitrogen, total; PC; Piston corer; Pyroxene/standard ratio; Quartz/standard ratio; Sampling/drilling in lake; Sand; Silt; Size fraction 〈 0.002 mm, clay; Size fraction 〉 2 mm, gravel; Sulfur, total; TaylorValley2002; Volcanic glass; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 3255 data points
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  • 12
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wagner, Bernd; Melles, Martin; Doran, Peter T; Kenig, Fabien; Forman, Steven L; Pierau, Roberto; Allen, Phillip (2006): Glacial and postglacial sedimentation in the Fryxell basin, Taylor Valley, southern Victoria Land, Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 241, 320-337, https://doi.org/10.1016/j.palaeo.2006.04.003
    Publication Date: 2023-10-28
    Description: A 9.14 m long sediment sequence was recovered from Lake Fryxell, Taylor Valley, southern Victoria Land, Antarctica, and investigated for its chronology and sedimentological, mineralogical, and biogeochemical changes. The basal part of the sequence is dominated by coarse clastic matter, i.e., mainly sand. The sediment composition suggests that a lake existed in Fryxell basin during the Middle Weichselian by ca. 48,000 cal. year BP. After a short period of lake-level lowstand ca. 43,000 cal. year BP, lower Taylor Valley became occupied by the proglacial Lake Washburn, which was at least partly supplied by meltwater and sediments from the Ross Ice Sheet that was advanced to the mouth of Taylor Valley. Evaporation of Lake Washburn to lower levels started during the Last Glacial Maximum at ca. 22,000 cal. year BP, long before the Ross Ice Sheet retreated significantly. Lake-level lowering was discontinuous with a series of high and low stands. From ca. 4000 cal. year BP environmental conditions were similar to those of today and lower Fryxell basin was occupied by a small lake. This lake evaporated to a saline or hypersaline pond between ca. 2500 and 1000 cal. year BP and refilled subsequently.
    Keywords: GC; Gravity corer; Lake Fryxell, East Antarctica; Lz1021; Lz1021-1; Lz1021-2; Lz1021-3; Lz1021-4; Lz1021-5; Lz1021-6; Lz1021-7; PC; Piston corer; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sampling/drilling in lake; SPP1158; TaylorValley2002
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 13
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Allogromiina sp.; Alveolophragmium crassimargo; Ammodiscus sp.; Ammotium cassis; Astrononion gallowayi; Biomass; Bolivina pseudopunctata; Buccella frigida; Cassidulina reniforme; Cibicides lobatulus; Cornuspira sp.; Counting 〉63 µm fraction; Cribrostomoides jeffreysii; DATE/TIME; Dentalina baggi; Depth, bathymetric; DEPTH, sediment/rock; Distance; ECHO; Echosounder; Eggerella advena; Elphidium clavatum; Elphidium subarcticum; Foraminifera, benthic, standing stock; Foraminifera, benthic calcareous; Foraminifera, benthic living; Globobulimina turgida; Grain size, sieving; Hippocrepinella alba; Hyperammina subnodosa; Islandiella helenae; Lagena semilineata; LATITUDE; LONGITUDE; Miliolinella sp.; Nonionellina labradorica; Number of species; Pelosina variabilis; Protelphidium orbiculare; Proteonina sp.; Psammosphaera sp.; Quinqueloqulina stalkeri; Recurvoides turbinatus; Reophax arcticus; Reophax atlantica; Reophax scorpiurus; Reophax scotti; Robertina arctica; Rosalina sp.; Sample code/label; Sand; Spiroplectammina biformis; Stainforthia loeblichi; Stainforthia schreibersiana; Trifarina fluens; Trochammina nana; Trochamminella bullata
    Type: Dataset
    Format: text/tab-separated-values, 396 data points
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  • 14
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Allogromiina sp.; Alveolophragmium crassimargo; Ammodiscus sp.; Ammotium cassis; Astrononion gallowayi; Bolivina pseudopunctata; Buccella frigida; Cassidulina reniforme; Cibicides lobatulus; Cornuspira sp.; Counting 〉63 µm fraction; Cribrostomoides jeffreysii; DATE/TIME; Dentalina baggi; Depth, bathymetric; DEPTH, sediment/rock; ECHO; Echosounder; Eggerella advena; Elphidium clavatum; Elphidium subarcticum; Foraminifera, benthic calcareous; Foraminifera, benthic dead; Foraminifera, benthic live/live+dead ratio; Foraminifera, benthic specimens; Globobulimina turgida; Hippocrepinella alba; Hyperammina subnodosa; Islandiella helenae; Lagena semilineata; LATITUDE; LONGITUDE; Miliolinella sp.; Nonionellina labradorica; Number of species; Pelosina variabilis; Protelphidium orbiculare; Proteonina sp.; Psammosphaera sp.; Quinqueloqulina stalkeri; Recurvoides turbinatus; Reophax arcticus; Reophax atlantica; Reophax scorpiurus; Reophax scotti; Robertina arctica; Rosalina sp.; Sample code/label; Spiroplectammina biformis; Stainforthia loeblichi; Stainforthia schreibersiana; Trifarina fluens; Trochammina nana; Trochamminella bullata
    Type: Dataset
    Format: text/tab-separated-values, 384 data points
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  • 15
    Publication Date: 2024-02-06
    Keywords: Abies; Alnus fruticosa; Alnus sp.; Apiaceae; Artemisia; Asteraceae; AWI_PerDyn; Betula sect. Albae-type; Betula sect. Nanae-type; Botrychium; Brassicaceae; Bryales; Cape Shpindler, Yugorski Peninsula, Russia; Carpinus; Caryophyllaceae; Chenopodiaceae; Cichoriaceae; Corylus; Counting, palynology; CS98-10; Cyperaceae; DEPTH, sediment/rock; Encalypta; Equisetum; Ericales; Fabaceae; Geological profile sampling; GEOPRO; Geranium; Huperzia selago-type; Juglans; Lamiaceae; Larix; Liliaceae; Lycopodium annotinum-type; Lycopodium clavatum; Lycopodium sp.; Myriophyllum; Onagraceae; Pediastrum; Permafrost Research (Periglacial Dynamics) @ AWI; Picea; Pinaceae; Pinus subgen. Diploxylon; Pinus subgen. Haploxylon; Plantago; Poaceae; Polemonium; Pollen indeterminata; Polygonum viviparum-type; Polypodiaceae; Primulaceae; Quaternary Environment of the Eurasian North; QUEEN; Ranunculaceae; Rosaceae; Rubus chamaemorus; Rumex/Oxyria-type; Salix; Saxifraga; Scrophulariaceae; Selaginella sibirica; Sphagnum; Thalictrum; Tilia; Typha; Ulmus sp.; Valeriana
    Type: Dataset
    Format: text/tab-separated-values, 2204 data points
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  • 16
    Publication Date: 2024-02-06
    Keywords: Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard deviation; AWI_PerDyn; Cape Shpindler, Yugorski Peninsula, Russia; CS98-10; DEPTH, sediment/rock; Geological profile sampling; GEOPRO; Permafrost Research (Periglacial Dynamics) @ AWI; Quaternary Environment of the Eurasian North; QUEEN; Sample, optional label/labor no
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 17
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Andreev, Andrei A; Manley, William F; Ingólfsson, Ólafur; Forman, Steven L (2001): Environmental changes on Yugorski Peninsula, Kara Sea, Russia, during the last 12,800 radiocarbon years. Global and Planetary Change, 31(1-4), 255-264, https://doi.org/10.1016/S0921-8181(01)00123-0
    Publication Date: 2024-02-06
    Description: New pollen and radiocarbon data from an 8.6-m coastal section, Cape Shpindler (69°43' N; 62°48' E), Yugorski Peninsula, document the latest Pleistocene and Holocene environmental history of this low Arctic region. Twelve AMS 14C dates indicate that the deposits accumulated since about 13,000 until 2000 radiocarbon years BP. A thermokarst lake formed ca. 13,000-12,800 years BP, when scarce arctic tundra vegetation dominated the area. By 12,500 years BP, a shallow lake existed at the site, and Arctic tundra with Poaceae, Cyperaceae, Salix, Saxifraga, and Artemisia dominated nearby vegetation. Climate was colder than today. Betula nana became dominant during the Early Preboreal period about 9500 years BP, responding to a warm event, which was one of the warmest during the Holocene. Decline in B. nana and Salix after 9500 years BP reflects a brief event of Preboreal cooling. A subsequent increase in Betula and Alnus fruticosa pollen percentages reflects amelioration of environmental conditions at the end of Preboreal period (ca. 9300 years BP). A decline in arboreal taxa later, with a dramatic increase in herb taxa, reflects a short cold event at about 9200 years BP. The pollen data reflect a northward movement of tree birch, peaking at the middle Boreal period, around 8500 years BP. Open Betula forest existed on the Kara Sea coast of the Yugorski Peninsula during the Atlantic period (8000-4500 years BP), indicating that climate was significantly warmer than today. Deteriorating climate around the Atlantic-Subboreal boundary (ca. 4500 years BP) is recorded by a decline in Betula percentages. Sedimentation slowed at the site, and processes of denudation and/or soil formation started at the beginning of the Subatlantic period, when vegetation cover on Yugorski Peninsula shifted to near-modern assemblages.
    Keywords: AWI_PerDyn; Cape Shpindler, Yugorski Peninsula, Russia; CS98-10; Geological profile sampling; GEOPRO; Permafrost Research (Periglacial Dynamics) @ AWI; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 18
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 22 (2003), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Glacier activity at Russkaya Gavan', north-west Novaya Zemlya (Arctic Russia), is reconstructed by particle size analysis of three fjord sediment cores in combination with 14C and 210Pb dating. Down-core logging of particle size variation reveals at least two intervals with sediment coarsening during the past eight centuries. By comparing them with reconstructions of summer temperature and atmospheric circulation, these intervals are interpreted to represent two cycles of glacier advance and retreat sometime during ca. AD 1400–1700 and AD 1700–present. Sediment accumulation thus appears to be sensitive to century-scale fluctuations of the Barents Sea climate. The identification of two glacier cycles in the glaciomarine record from Russkaya Gavan’ demonstrates that during the “Little Ice Age” major glacier fluctuations on Novaya Zemlya occurred in broad synchrony with those in other areas around the Barents Sea.
    Type of Medium: Electronic Resource
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  • 19
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 5 (1987), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Type of Medium: Electronic Resource
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  • 20
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 11 (1992), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Five species of guide fossils from the Holocene warm period in Svalbard are considered: Mytilus edulis, Modiolus modiolus, Arctica islandica, Littorina littorea and Zirphaea crispata. These are now extinct in Svalbard; Zirphaea crispata, especially, requires considerable higher water temperatures than occur there today. Known radiocarbon dates on Mytilus, Modiolus and Zirphala are given. Thirty-four dates on Mytilus edulis show that it lived in Svalbard from before 9500 BP to about 3500 BP, and probably again around 1000 BP. Five dates on Modiolus and Zirphaea indicate a climatic optimum in Svalbard from about 8700 BP to 7700 BP. The most favourable places then had conditions similar to the northeastern coast of Finnmark, northernmost Norway, today. Mytilus edulis is considered a good climate indicator, and a future warming of the marine climate in Svalbard could be indicated by its eventual re-immigration into the area.
    Type of Medium: Electronic Resource
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