Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.

Limnopolar Lake, Livingston Island, situated close to the tip of the northern Antarctic Peninsula (62°40'S, 61°00'W), has experienced a long history of primary and secondary tephra inputs from nearby volcanic centres. Background levels of tephra in a sediment core collected from the lake w...

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Main Author: Agius, JT
Format: Thesis
Language:English
Published: Honours thesis, University of Tasmania 2006
Subjects:
Online Access:https://eprints.utas.edu.au/8815/
https://eprints.utas.edu.au/8815/2/agiusThesis.2.pdf
id ftunivtasmania:oai:eprints.utas.edu.au:8815
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:8815 2023-05-15T13:36:46+02:00 Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island. Agius, JT 2006 application/pdf https://eprints.utas.edu.au/8815/ https://eprints.utas.edu.au/8815/2/agiusThesis.2.pdf en eng Honours thesis, University of Tasmania https://eprints.utas.edu.au/8815/2/agiusThesis.2.pdf Agius, JT 2006 , 'Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.', Honours thesis, University of Tasmania. cc_utas Thesis NonPeerReviewed 2006 ftunivtasmania 2020-05-30T07:22:33Z Limnopolar Lake, Livingston Island, situated close to the tip of the northern Antarctic Peninsula (62°40'S, 61°00'W), has experienced a long history of primary and secondary tephra inputs from nearby volcanic centres. Background levels of tephra in a sediment core collected from the lake were ~30,000-35,000 gdm-1, and were caused by the continual washing in of tephra deposited in the surrounding watershed. Tephra abundances above these levels were assigned to tephra horizons, of which 5 were identified to have occurred over the last 2000 years. Electron probe microanalysis of the tephra shards revealed that the predominant composition of the tephra was basaltic andesite, with few basalt and andesite pyroclasts. Limited numbers of shards with trachy-basalt and basaltic trachy-andesite compositions were also recorded. Deception Island was attributed as the most likely source of the tephra. Eight distinct biological communities were identified in the sediment core on the basis of abundance and distribution of organism remains. Most community shifts over the last ~2000 years appear to be due to direct or indirect effects of tephra deposition into the lake, with tephra abundance levels being an important factor. However, some community shifts can be attributed to climate variability and grazing pressures. The apparent lack of zooplankton species, with only a recent colonisation of the anostracan Branchinecta gainii and possibly the copepod Boeckella poppei, suggests that zooplankton species may not be adapted to surviving in lakes with continual tephral inputs or alternately have recently colonised the island. Thesis Antarc* Antarctic Antarctic Peninsula Deception Island Livingston Island University of Tasmania: UTas ePrints Antarctic Antarctic Peninsula Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950) Livingston Island ENVELOPE(-60.500,-60.500,-62.600,-62.600) Byers ENVELOPE(-60.283,-60.283,-63.900,-63.900) Boeckella ENVELOPE(-56.999,-56.999,-63.404,-63.404) Byers peninsula ENVELOPE(-61.066,-61.066,-62.633,-62.633) Limnopolar Lake ENVELOPE(-61.098,-61.098,-62.633,-62.633)
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
description Limnopolar Lake, Livingston Island, situated close to the tip of the northern Antarctic Peninsula (62°40'S, 61°00'W), has experienced a long history of primary and secondary tephra inputs from nearby volcanic centres. Background levels of tephra in a sediment core collected from the lake were ~30,000-35,000 gdm-1, and were caused by the continual washing in of tephra deposited in the surrounding watershed. Tephra abundances above these levels were assigned to tephra horizons, of which 5 were identified to have occurred over the last 2000 years. Electron probe microanalysis of the tephra shards revealed that the predominant composition of the tephra was basaltic andesite, with few basalt and andesite pyroclasts. Limited numbers of shards with trachy-basalt and basaltic trachy-andesite compositions were also recorded. Deception Island was attributed as the most likely source of the tephra. Eight distinct biological communities were identified in the sediment core on the basis of abundance and distribution of organism remains. Most community shifts over the last ~2000 years appear to be due to direct or indirect effects of tephra deposition into the lake, with tephra abundance levels being an important factor. However, some community shifts can be attributed to climate variability and grazing pressures. The apparent lack of zooplankton species, with only a recent colonisation of the anostracan Branchinecta gainii and possibly the copepod Boeckella poppei, suggests that zooplankton species may not be adapted to surviving in lakes with continual tephral inputs or alternately have recently colonised the island.
format Thesis
author Agius, JT
spellingShingle Agius, JT
Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
author_facet Agius, JT
author_sort Agius, JT
title Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
title_short Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
title_full Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
title_fullStr Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
title_full_unstemmed Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.
title_sort tephra and ecological studies of limnopolar lake, byers peninsula, livingston island.
publisher Honours thesis, University of Tasmania
publishDate 2006
url https://eprints.utas.edu.au/8815/
https://eprints.utas.edu.au/8815/2/agiusThesis.2.pdf
long_lat ENVELOPE(-60.633,-60.633,-62.950,-62.950)
ENVELOPE(-60.500,-60.500,-62.600,-62.600)
ENVELOPE(-60.283,-60.283,-63.900,-63.900)
ENVELOPE(-56.999,-56.999,-63.404,-63.404)
ENVELOPE(-61.066,-61.066,-62.633,-62.633)
ENVELOPE(-61.098,-61.098,-62.633,-62.633)
geographic Antarctic
Antarctic Peninsula
Deception Island
Livingston Island
Byers
Boeckella
Byers peninsula
Limnopolar Lake
geographic_facet Antarctic
Antarctic Peninsula
Deception Island
Livingston Island
Byers
Boeckella
Byers peninsula
Limnopolar Lake
genre Antarc*
Antarctic
Antarctic Peninsula
Deception Island
Livingston Island
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Deception Island
Livingston Island
op_relation https://eprints.utas.edu.au/8815/2/agiusThesis.2.pdf
Agius, JT 2006 , 'Tephra and ecological studies of Limnopolar Lake, Byers Peninsula, Livingston Island.', Honours thesis, University of Tasmania.
op_rights cc_utas
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