GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • PANGAEA  (418)
  • Alfred Wegener Institute for Polar and Marine Research  (4)
  • Amsterdam [u.a.] : Elsevier  (1)
Document type
Keywords
Language
Years
  • 1
    Keywords: Estuarine sediments Research ; Russia (Federation) ; Kara Sea ; Runoff Environmental aspects ; Russia (Federation) ; Kara Sea ; Seawater Organic compound content ; Marine ecology Russia (Federation) ; Kara Sea ; estuarine sediments ; runoff ; environmental aspects ; seawater, Organic compound content ; marine ecology ; Russia (Federation) ; Kara Sea ; Aufsatzsammlung ; Sibirien Nord ; Abflussregime ; Flusslandschaft ; Flusssystem ; Umweltfaktor ; Nordpolarmeer ; Karasee ; Fluss ; Mündung ; Unterlauf ; Fluviale Sedimentation ; Sibirien Nord ; Abflussregime ; Flusslandschaft ; Flusssystem ; Umweltfaktor ; Nordpolarmeer ; Karasee ; Fluss ; Mündung ; Unterlauf ; Fluviale Sedimentation
    Type of Medium: Book
    Pages: VII, 488 S , graph. Darst , 1 Beil. (Ber.-Bl.)
    Edition: 1. ed.
    ISBN: 0444513655
    Series Statement: Proceedings in marine science 6
    DDC: 551.461325
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Méheust, Marie; Stein, Ruediger; Fahl, Kirsten; Max, Lars; Riethdorf, Jan-Rainer (2015): High-resolution IP25-based reconstruction of sea-ice variability in the western North Pacific and Bering Sea during the past 18,000 years. Geo-Marine Letters, https://doi.org/10.1007/s00367-015-0432-4
    Publication Date: 2023-03-16
    Description: Due to its strong influence on heat and moisture exchange between the ocean and the atmosphere, sea ice is an essential component of the global climate system. In the context of its alarming decrease in terms of concentration, thickness and duration, understanding the processes controlling sea-ice variability and reconstructing paleo-sea-ice extent in polar regions have become of great interest for the scientific community. In this study, for the first time, IP25, a recently developed biomarker sea-ice proxy, was used for a high-resolution reconstruction of the sea-ice extent and its variability in the western North Pacific and western Bering Sea during the past 18,000 years. To identify mechanisms controlling the sea-ice variability, IP25 data were associated with published sea-surface temperature as well as diatom and biogenic opal data. The results indicate that a seasonal sea-ice cover existed during cold periods (Heinrich Stadial 1 and Younger Dryas), whereas during warmer intervals (Bølling-Allerød and Holocene) reduced sea ice or ice-free conditions prevailed in the study area. The variability in sea-ice extent seems to be linked to climate anomalies and sea-level changes controlling the oceanographic circulation between the subarctic Pacific and the Bering Sea, especially the Alaskan Stream injection though the Aleutian passes.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Stein, Ruediger; Fahl, Kirsten; Gierz, Paul; Niessen, Frank; Lohmann, Gerrit (2017): Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial. Nature Communications, 8(1), 13 pp, https://doi.org/10.1038/s41467-017-00552-1
    Publication Date: 2023-03-16
    Description: Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four decades and climate scenarios suggest that sea ice may completely disappear during summer within the next about 50-100 years. Here we produce Arctic sea ice biomarker proxy records for the penultimate glacial (Marine Isotope Stage 6) and the subsequent last interglacial (Marine Isotope Stage 5e). The latter is a time interval when the high latitudes were significantly warmer than today. We document that even under such warmer climate conditions, sea ice existed in the central Arctic Ocean during summer, whereas sea ice was significantly reduced along the Barents Sea continental margin influenced by Atlantic Water inflow. Our proxy reconstruction of the last interglacial sea ice cover is supported by climate simulations, although some proxy data/model inconsistencies still exist. During late Marine Isotope Stage 6, polynya-type conditions occurred off the major ice sheets along the northern Barents and East Siberian continental margins, contradicting a giant Marine Isotope Stage 6 ice shelf that covered the entire Arctic Ocean.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-03-16
    Description: Past sea ice conditions and open water phytoplankton production were reconstructed from a sediment core taken in Disko Bugt, West Greenland, using the sea ice biomarker IP~25~ and other specific phytoplankton biomarker (i.e., brassicasterol, dinosterol, HBI III) records. Our biomarker record indicates that Disko Bugt experienced a gradual expansion of seasonal sea ice during the last 2.2 kyr. Maximum sea ice extent was reached during the Little Ice Age around 0.2 kyr BP. Superimposed on this longer term trend, we find short-term oscillations in open water primary production and terrigenous input, which may be related to the Atlantic Multidecadal Oscillation and solar activity changes as potential climatic trigger mechanisms. A direct sample-to-sample multiproxy comparison of our new biomarker record with microfossil (i.e., benthic foraminifera, dinocysts, and diatoms) and other geochemical records (i.e., alkenone biomarkers) indicates that different proxies are influenced by the complex environmental system with pronounced seasonal changes and strong oceanographic gradients, e.g., freshwater inflow from the Greenland Ice Sheet. Differences in sea ice reconstructions may indicate that the IP~25~ record reflects only the relatively short sea ice season (spring), whereas other microfossil reconstructions may reflect a longer (spring–autumn) interval.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten (2018): Paleo-sea ice distribution and polynya variability on the Kara sea shelf during the last 12 ka. arktos - The Journal of Arctic Geosciences, https://doi.org/10.1007/s41063-018-0040-4
    Publication Date: 2023-03-16
    Description: The Kara Sea is an important area for paleo-climatic research since sea ice and brine formation take place on its shelf-two processes inducing supra-regional climatic implications and thereby connecting regional environmental variability with global climatic conditions. To gain information about past sea ice coverage and variations, three sediment cores distributed in the southern and central parts of the marginal Sea were investigated. By applying the sea ice biomarker IP25 and the PIP25 index [phytoplankton biomarker (dinosterol)-IP25 index] post-glacial sea ice variability could be detected in the central Kara Sea (Core BP00-36/4), with most intense sea ice cover between 12.4 and 11.8 ka coinciding with the Younger Dryas (12.9-11.6 ka), and reduced sea ice cover between 10 and 8 ka during the Holocene Thermal Maximum. During the last ~7 ka, increasing sea ice indicators might indicate a Holocene cooling trend, probably induced by declining summer insolation. Furthermore, temporal changes in the fast ice?polynya distribution in the southern Kara Sea were detected: expanding fast ice during the late Holocene and a cyclic short-term Holocene climate variability documented by abrupt changes in the sea ice coverage at the BP00-07/7 core site. Core BP99-04/7 from the Yenisei estuary recorded consistently seasonal sea ice cover since ~9.3 ka, apart from five short phases of fast ice expansion to the core site. The strong influence of river run-off as well as estuary processes might prevent the detection of (short-term) climatic signals at this study site.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2023-03-16
    Keywords: 4380-3; 4382-4; 4386-7; 4388-3; 4391-2; 4399-1; 4403-1; 4411-1; 4413-1; 4414-1; 4416-1; 4417-2; 4418-1; BC; Box corer; Carbon, organic, total; DEPTH, sediment/rock; DM49; Dmitry Mendeleev; Element analyser CHN, LECO; Elevation of event; Event label; Jenissei; KAL_R; Kasten corer RUS; Latitude of event; Longitude of event; Men4380-3; Men4382-4; Men4386-7; Men4388-3; Men4391-2; Men4399-1; Men4403-1; Men4409-1; Men4410-1; Men4411-1; Men4413-1; Men4414-1; Men4416-1; Men4417-2; Men4418-1; Ob; Siberian River Run-Off; SIRRO; SPASIBAIII; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2023-03-16
    Keywords: 4380-3; 4382-4; 4386-7; 4388-3; 4391-2; 4399-1; 4403-1; 4411-1; 4413-1; 4414-1; 4416-1; 4417-2; 4418-1; BC; Box corer; Carbon/Nitrogen ratio; DEPTH, sediment/rock; DM49; Dmitry Mendeleev; Elevation of event; Event label; Jenissei; KAL_R; Kasten corer RUS; Latitude of event; Longitude of event; Men4380-3; Men4382-4; Men4386-7; Men4388-3; Men4391-2; Men4399-1; Men4403-1; Men4409-1; Men4410-1; Men4411-1; Men4413-1; Men4414-1; Men4416-1; Men4417-2; Men4418-1; Ob; Siberian River Run-Off; SIRRO; SPASIBAIII; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-03-16
    Keywords: AWI_BioOce; Biogenic, flux; Biological Oceanography @ AWI; Calcium carbonate, flux; Carbon, organic, particulate, flux; DATE/TIME; DEPTH, water; Duration, number of days; Elevation of event; Event label; FRAM; FRontiers in Arctic marine Monitoring; Gakkel_A1-1; Gakkel_N1-1; Latitude of event; Lithogenic, flux; Longitude of event; MOOR; Mooring; PS78/255-1; PS78/262-3; Seston, flux; Silicon, dissolved + particulate, flux
    Type: Dataset
    Format: text/tab-separated-values, 518 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bartels, Martin; Titschack, Jürgen; Fahl, Kirsten; Stein, Ruediger; Seidenkrantz, Marit-Solveig; Hillaire-Marcel, Claude; Hebbeln, Dierk (2017): Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation. Climate of the Past Discussions, 13, 1717-1749, https://doi.org/10.5194/cp-13-1717-2017
    Publication Date: 2023-03-03
    Description: Atlantic Water (AW) advection plays an important role for climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic Ocean, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection history and document its linkage with local glacier dynamics, as illustrated in the present study of a 275 cm long sedimentary record from Woodfjorden (northern Spitsbergen; water depth: 171 m) spanning the last ~15,500 years. Sedimentological, micropalaeontological and geochemical analyses were used to reconstruct changes in marine environmental conditions, sea-ice cover and glacier activity. Data illustrate a partial breakup of the Svalbard-Barents Sea Ice Sheet from Heinrich Stadial 1 onwards (until ~14.6 ka). During the Bølling-Allerød (~14.6-12.7 ka), AW penetrated as a bottom water mass into the fjord system and contributed significantly to the destabilisation of local glaciers. During the Younger Dryas (~12.7-11.7 ka), it intruded into intermediate waters while evidence for a glacier advance is lacking. A short-term deepening of the halocline occurred at the very end of this interval. During the early Holocene (~11.7-7.8 ka), mild conditions led to glacier retreat, a reduced sea-ice cover and increasing sea surface temperatures, with a brief interruption during the Preboreal Oscillation (~11.1-10.8 ka). Due to a ~6,000-years gap, the mid-Holocene is not recorded in this sediment core. During the late Holocene (~1.8-0.4 ka), a slightly reduced AW inflow and lower sea surface temperatures compared to the early Holocene are reconstructed. Glaciers, which previously retreated to the shallower inner parts of the Woodfjorden system, likely advanced during the late Holocene. In particular, as topographic control in concert with the reduced summer insolation partly decoupled glacier dynamics from AW advection during this recent interval.
    Keywords: Center for Marine Environmental Sciences; GeoB; Geosciences, University of Bremen; MARUM
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bartels, Martin; Titschack, Jürgen; Fahl, Kirsten; Stein, Ruediger; Hebbeln, Dierk (2018): Wahlenbergfjord, eastern Svalbard: a glacier-surrounded fjord reflecting regional hydrographic variability during the Holocene? Boreas, 47(4), 1003-1021, https://doi.org/10.1111/bor.12325
    Publication Date: 2023-03-03
    Description: Exceptionally high sedimentation rates in Arctic fjords provide the possibility to reconstruct environmental conditions in high temporal resolution during the (pre-)Holocene. The unique geographical location of Svalbard at the intersection of Arctic and Atlantic waters offers the opportunity to estimate local (mainly glacier-related) vs. regional (hydrographic) variabilities. Sedimentological, micropalaeontological and geochemical data from the very remote, glacier-surrounded Wahlenbergfjord in eastern Svalbard provides information on glacier dynamics, palaeoceanographic and sea ice conditions during the Holocene. The present study illustrates a high meltwater discharge during the summer insolation maximum (~11.3-7.7 ka) when the intrusion of upwelled relatively warm Atlantic-derived waters led to an almost open fjord situation with reduced sea ice in summer. Around 7.7 ka, a rapid hydrographic shift occurred: The dominance of inflowing Atlantic-derived waters was replaced by a stronger influence of Arctic Water reflecting regional palaeoceanographic conditions evident in the benthic foraminiferal fauna also at Svalbard's margins. Neoglacial conditions characterised the late Holocene (~3.1-0.2 ka), when glaciers likely advanced as cold atmospheric temperatures were decoupled from the advection of relatively warm intermediate waters probably caused by an extending sea ice coverage. Accordingly, our data show that even a remote, glacier-proximal study site reflects rapid as well as longer-term regional changes.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...