Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations

The North Lake Lobe of the Quelccaya Ice Cap in southern Peru represents a wholly unique location for reconstructing paleoclimate conditions. At this location, plant samples were preserved in-situ beneath the advancing glacial ice, and since 2004 have been collected as the ice retreats. The ages of...

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Main Author: Stahl, Henry
Other Authors: Thompson, Lonnie
Format: Thesis
Language:English
Published: The Ohio State University 2017
Subjects:
ice
Online Access:http://hdl.handle.net/1811/80465
id ftohiostateu:oai:kb.osu.edu:1811/80465
record_format openpolar
spelling ftohiostateu:oai:kb.osu.edu:1811/80465 2023-05-15T16:39:22+02:00 Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations Stahl, Henry Thompson, Lonnie 2017-05 application/pdf http://hdl.handle.net/1811/80465 en_US eng The Ohio State University The Ohio State University. School of Earth Sciences Undergraduate Research Theses; 2017 http://hdl.handle.net/1811/80465 radiocarbon plant ice Quelccaya Holocene carbon-14 Thesis 2017 ftohiostateu 2020-08-22T19:21:57Z The North Lake Lobe of the Quelccaya Ice Cap in southern Peru represents a wholly unique location for reconstructing paleoclimate conditions. At this location, plant samples were preserved in-situ beneath the advancing glacial ice, and since 2004 have been collected as the ice retreats. The ages of the collected samples were obtained through radiocarbon dating methods. Samples were collected at the surface and at depth. The fine-grained nature of the matrix surrounding the preserved buried samples indicates that several flood events occurred at these sites between ~6,630 cal yr BP and ~6450 cal yr BP due to the ice damming of a lake above the sites. The temporal relationships of the samples were analyzed using a density kernel derivative function, and several groups of significantly related surface samples were determined. We were then able to map several successive advancing ice margins from ~6431 cal yr BP to ~4565 cal yr BP using the temporospatial data of the different sample groups. Comparing the findings of the advancing ice margins to regional climatic records, we determined that the principal driver of the Quelccaya Ice Cap behavior is temperature change, rather than changes in precipitation. Therefore, the advancement seen at the North Lake Lobe of the Quelccaya Ice Cap is another indicator of cooling regional temperatures in South America during the mid-Holocene. When compared to extensive temperature records from locations around the world, the North Lake Lobe advancement supports the hypothesis that a global cooling event occurred during the mid-Holocene. National Science Foundation RAPID Grant Award #1603377 National Science Foundation Paleoclimate Program Award ATM-0318430 Ohio State University Climate, Water, and Carbon Program Ohio State University Office of Research Ohio State College of Arts and Sciences Byrd Polar and Climate Research Center Ice Core Paleoclimate Research Endowment No embargo Academic Major: Earth Sciences Thesis ice core Ohio State University (OSU): Knowledge Bank Byrd
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
topic radiocarbon
plant
ice
Quelccaya
Holocene
carbon-14
spellingShingle radiocarbon
plant
ice
Quelccaya
Holocene
carbon-14
Stahl, Henry
Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
topic_facet radiocarbon
plant
ice
Quelccaya
Holocene
carbon-14
description The North Lake Lobe of the Quelccaya Ice Cap in southern Peru represents a wholly unique location for reconstructing paleoclimate conditions. At this location, plant samples were preserved in-situ beneath the advancing glacial ice, and since 2004 have been collected as the ice retreats. The ages of the collected samples were obtained through radiocarbon dating methods. Samples were collected at the surface and at depth. The fine-grained nature of the matrix surrounding the preserved buried samples indicates that several flood events occurred at these sites between ~6,630 cal yr BP and ~6450 cal yr BP due to the ice damming of a lake above the sites. The temporal relationships of the samples were analyzed using a density kernel derivative function, and several groups of significantly related surface samples were determined. We were then able to map several successive advancing ice margins from ~6431 cal yr BP to ~4565 cal yr BP using the temporospatial data of the different sample groups. Comparing the findings of the advancing ice margins to regional climatic records, we determined that the principal driver of the Quelccaya Ice Cap behavior is temperature change, rather than changes in precipitation. Therefore, the advancement seen at the North Lake Lobe of the Quelccaya Ice Cap is another indicator of cooling regional temperatures in South America during the mid-Holocene. When compared to extensive temperature records from locations around the world, the North Lake Lobe advancement supports the hypothesis that a global cooling event occurred during the mid-Holocene. National Science Foundation RAPID Grant Award #1603377 National Science Foundation Paleoclimate Program Award ATM-0318430 Ohio State University Climate, Water, and Carbon Program Ohio State University Office of Research Ohio State College of Arts and Sciences Byrd Polar and Climate Research Center Ice Core Paleoclimate Research Endowment No embargo Academic Major: Earth Sciences
author2 Thompson, Lonnie
format Thesis
author Stahl, Henry
author_facet Stahl, Henry
author_sort Stahl, Henry
title Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
title_short Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
title_full Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
title_fullStr Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
title_full_unstemmed Carbon-14 Plant Evidence of mid-Holocene Quelccaya Ice Cap Margin Fluctuations
title_sort carbon-14 plant evidence of mid-holocene quelccaya ice cap margin fluctuations
publisher The Ohio State University
publishDate 2017
url http://hdl.handle.net/1811/80465
geographic Byrd
geographic_facet Byrd
genre ice core
genre_facet ice core
op_relation The Ohio State University. School of Earth Sciences Undergraduate Research Theses; 2017
http://hdl.handle.net/1811/80465
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