Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...

The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes tha...

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Main Authors: Hass, H Christian, Kuhn, Gerhard, Monien, Patrick, Brumsack, Hans-Jürgen, Forwick, Matthias
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.788113
https://doi.pangaea.de/10.1594/PANGAEA.788113
id ftdatacite:10.1594/pangaea.788113
record_format openpolar
spelling ftdatacite:10.1594/pangaea.788113 2023-10-01T03:50:40+02:00 Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ... Hass, H Christian Kuhn, Gerhard Monien, Patrick Brumsack, Hans-Jürgen Forwick, Matthias 2010 application/zip https://dx.doi.org/10.1594/pangaea.788113 https://doi.pangaea.de/10.1594/PANGAEA.788113 en eng PANGAEA https://dx.doi.org/10.1144/sp344.17 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Supplementary Publication Series of Datasets article Collection 2010 ftdatacite https://doi.org/10.1594/pangaea.78811310.1144/sp344.17 2023-09-04T14:52:34Z The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern ... : Supplement to: Hass, H Christian; Kuhn, Gerhard; Monien, Patrick; Brumsack, Hans-Jürgen; Forwick, Matthias (2010): Climate fluctuations during the past two millennia as recorded in sediments from Maxwell Bay, South Shetland Islands, West Antarctica. In: Howe, J; Austin, WEN; Paetzel, M and Forwick, M (eds.): Fjordic Depositional Systems and Archives, Geological Society of London Special Publication, 344, 243-260 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Arctic King George Island Maxwell Bay Sea ice South Shetland Islands West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic Austin King George Island Maxwell Bay ENVELOPE(-58.859,-58.859,-62.223,-62.223) South Shetland Islands West Antarctica
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
spellingShingle Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
Hass, H Christian
Kuhn, Gerhard
Monien, Patrick
Brumsack, Hans-Jürgen
Forwick, Matthias
Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
topic_facet Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
description The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern ... : Supplement to: Hass, H Christian; Kuhn, Gerhard; Monien, Patrick; Brumsack, Hans-Jürgen; Forwick, Matthias (2010): Climate fluctuations during the past two millennia as recorded in sediments from Maxwell Bay, South Shetland Islands, West Antarctica. In: Howe, J; Austin, WEN; Paetzel, M and Forwick, M (eds.): Fjordic Depositional Systems and Archives, Geological Society of London Special Publication, 344, 243-260 ...
format Article in Journal/Newspaper
author Hass, H Christian
Kuhn, Gerhard
Monien, Patrick
Brumsack, Hans-Jürgen
Forwick, Matthias
author_facet Hass, H Christian
Kuhn, Gerhard
Monien, Patrick
Brumsack, Hans-Jürgen
Forwick, Matthias
author_sort Hass, H Christian
title Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
title_short Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
title_full Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
title_fullStr Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
title_full_unstemmed Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica ...
title_sort granulometry of two sediment cores from maxwell bay, south shetland islands, west antarctica ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.788113
https://doi.pangaea.de/10.1594/PANGAEA.788113
long_lat ENVELOPE(-58.859,-58.859,-62.223,-62.223)
geographic Antarctic
Arctic
Austin
King George Island
Maxwell Bay
South Shetland Islands
West Antarctica
geographic_facet Antarctic
Arctic
Austin
King George Island
Maxwell Bay
South Shetland Islands
West Antarctica
genre Antarc*
Antarctic
Antarctica
Arctic
King George Island
Maxwell Bay
Sea ice
South Shetland Islands
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Arctic
King George Island
Maxwell Bay
Sea ice
South Shetland Islands
West Antarctica
op_relation https://dx.doi.org/10.1144/sp344.17
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.78811310.1144/sp344.17
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