A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications
Island, shows that the lake and its catchment have undergone significant changes during the last 4000 years. Radiocarbon dating (AMS), sediment lithology, and microfossil analyses indicate that the lake was deglaciated over 4000 14C years ago. Distinct peaks in accumulation rates of sediment, Pedius...
Main Authors: | , , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1991
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.468.2241 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.468.2241 2023-05-15T14:05:25+02:00 A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications Svante Bjorck Hannelore Hskansson Rolf Zale Wibjorn Karlen The Pennsylvania State University CiteSeerX Archives 1991 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf Key words Antarctica I4C chronology lake sediments microfossil stratigraphy palaeoclimatology text 1991 ftciteseerx 2016-01-08T07:03:36Z Island, shows that the lake and its catchment have undergone significant changes during the last 4000 years. Radiocarbon dating (AMS), sediment lithology, and microfossil analyses indicate that the lake was deglaciated over 4000 14C years ago. Distinct peaks in accumulation rates of sediment, Pediustrum algae, pollen and spores, as well as changes in the diatom assemblage, suggest significant environmental changes between ca 3200 and 2700 y BP. These changes are interpreted as reflecting a milder and more humid, maritime climate. The increased humidity can explain independent observations of glacier growth during this period. The combined data also indicate that between ca 1500 and 500 y BP the area might have experienced morecontinental conditions with slightly colder and drier climate than today. Since the 14C dates from the Midge Lake sediments are regarded as reliable and the sediment sequence is rich in tephra layers this sediment sequence will be critical for a forthcoming tephra chronology of the region. Text Antarc* Antarctica South Shetland Islands Unknown South Shetland Islands Livingstone ENVELOPE(-134.337,-134.337,61.333,61.333) Livingstone Island ENVELOPE(-74.448,-74.448,71.718,71.718) Midge Lake ENVELOPE(-61.088,-61.088,-62.636,-62.636) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Key words Antarctica I4C chronology lake sediments microfossil stratigraphy palaeoclimatology |
spellingShingle |
Key words Antarctica I4C chronology lake sediments microfossil stratigraphy palaeoclimatology Svante Bjorck Hannelore Hskansson Rolf Zale Wibjorn Karlen A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
topic_facet |
Key words Antarctica I4C chronology lake sediments microfossil stratigraphy palaeoclimatology |
description |
Island, shows that the lake and its catchment have undergone significant changes during the last 4000 years. Radiocarbon dating (AMS), sediment lithology, and microfossil analyses indicate that the lake was deglaciated over 4000 14C years ago. Distinct peaks in accumulation rates of sediment, Pediustrum algae, pollen and spores, as well as changes in the diatom assemblage, suggest significant environmental changes between ca 3200 and 2700 y BP. These changes are interpreted as reflecting a milder and more humid, maritime climate. The increased humidity can explain independent observations of glacier growth during this period. The combined data also indicate that between ca 1500 and 500 y BP the area might have experienced morecontinental conditions with slightly colder and drier climate than today. Since the 14C dates from the Midge Lake sediments are regarded as reliable and the sediment sequence is rich in tephra layers this sediment sequence will be critical for a forthcoming tephra chronology of the region. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Svante Bjorck Hannelore Hskansson Rolf Zale Wibjorn Karlen |
author_facet |
Svante Bjorck Hannelore Hskansson Rolf Zale Wibjorn Karlen |
author_sort |
Svante Bjorck |
title |
A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
title_short |
A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
title_full |
A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
title_fullStr |
A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
title_full_unstemmed |
A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications |
title_sort |
late holocene lake sediment sequence from livingstone island, south shetland islands, with paleo-climatic implications |
publishDate |
1991 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf |
long_lat |
ENVELOPE(-134.337,-134.337,61.333,61.333) ENVELOPE(-74.448,-74.448,71.718,71.718) ENVELOPE(-61.088,-61.088,-62.636,-62.636) |
geographic |
South Shetland Islands Livingstone Livingstone Island Midge Lake |
geographic_facet |
South Shetland Islands Livingstone Livingstone Island Midge Lake |
genre |
Antarc* Antarctica South Shetland Islands |
genre_facet |
Antarc* Antarctica South Shetland Islands |
op_source |
http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766277321089613824 |