An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice

Alpine glaciers situated in mid- and low latitudes are valuable archives for paleoclimatology. They offer a continuous record of recent local climatic conditions in regions where the majority of humankind lived and still lives. For meaningful interpretation of an ice core from such an archive, accur...

Full description

Bibliographic Details
Main Author: Schindler, Johannes
Other Authors: Schwikowski, Margit
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 2017
Subjects:
Online Access:https://boris.unibe.ch/99695/1/17schindler_j.pdf
https://boris.unibe.ch/99695/
id ftunivbern:oai:boris.unibe.ch:99695
record_format openpolar
spelling ftunivbern:oai:boris.unibe.ch:99695 2023-08-20T04:07:12+02:00 An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice Schindler, Johannes Schwikowski, Margit 2017 application/pdf https://boris.unibe.ch/99695/1/17schindler_j.pdf https://boris.unibe.ch/99695/ eng eng https://boris.unibe.ch/99695/ info:eu-repo/semantics/openAccess Schindler, Johannes (2017). An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice. (Dissertation, Universität Bern, Philosophisch-naturwissenschaftliche Fakultät, Departement für Chemie und Biochemie) 570 Life sciences biology 540 Chemistry info:eu-repo/semantics/doctoralThesis info:eu-repo/semantics/publishedVersion NonPeerReviewed 2017 ftunivbern 2023-07-31T21:35:49Z Alpine glaciers situated in mid- and low latitudes are valuable archives for paleoclimatology. They offer a continuous record of recent local climatic conditions in regions where the majority of humankind lived and still lives. For meaningful interpretation of an ice core from such an archive, accurate dating is essential. Usually, several complementary approaches are used to establish a depth-age relationship. The oldest part of the ice at the bottom of the ice core suffers annual layer thinning and is influenced by small-scale bedrock geometry, which limits the use of annual layer counting or the assignment of reference horizons for dating. Nuclear dating techniques overcome this restriction since they do not rely on the preservation of a resolvable stratigraphy by using the continuous record of the respective radioisotope. Radiocarbon is especially powerful for dating alpine glaciers because its half-life of 5730 years suitably allows it to cover the typical age range of these archives. Most important, glacier ice does contain minute amounts of carbon. While macrofossils can only be found by coincidence, organic aerosols deposited on the glacier offer the best source of contemporary carbon in glacier ice. Despite a large part of its chemical composition being unknown, organic carbon found in an ice sample can be operationally classified into a particulate fraction (POC) and a dissolved fraction (DOC). Radiocarbon dating of POC has proven to be very successful and is a routine application by now. The major limitation of this technique is the low POC concentration found especially in pre-industrial and polar ice samples. Therefore, the DOC fraction promises even better suitability for dating thanks to its by a factor of 5 to 10 higher concentrations. Nevertheless, a straightforward analysis of DOC is hampered by its vulnerability to contamination. DOC consists in large part of mono- and dicarboxylic acids - compounds that can easily be taken up from the surrounding gas phase during sample preparation or which ... Doctoral or Postdoctoral Thesis ice core BORIS (Bern Open Repository and Information System, University of Bern)
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 570 Life sciences
biology
540 Chemistry
spellingShingle 570 Life sciences
biology
540 Chemistry
Schindler, Johannes
An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
topic_facet 570 Life sciences
biology
540 Chemistry
description Alpine glaciers situated in mid- and low latitudes are valuable archives for paleoclimatology. They offer a continuous record of recent local climatic conditions in regions where the majority of humankind lived and still lives. For meaningful interpretation of an ice core from such an archive, accurate dating is essential. Usually, several complementary approaches are used to establish a depth-age relationship. The oldest part of the ice at the bottom of the ice core suffers annual layer thinning and is influenced by small-scale bedrock geometry, which limits the use of annual layer counting or the assignment of reference horizons for dating. Nuclear dating techniques overcome this restriction since they do not rely on the preservation of a resolvable stratigraphy by using the continuous record of the respective radioisotope. Radiocarbon is especially powerful for dating alpine glaciers because its half-life of 5730 years suitably allows it to cover the typical age range of these archives. Most important, glacier ice does contain minute amounts of carbon. While macrofossils can only be found by coincidence, organic aerosols deposited on the glacier offer the best source of contemporary carbon in glacier ice. Despite a large part of its chemical composition being unknown, organic carbon found in an ice sample can be operationally classified into a particulate fraction (POC) and a dissolved fraction (DOC). Radiocarbon dating of POC has proven to be very successful and is a routine application by now. The major limitation of this technique is the low POC concentration found especially in pre-industrial and polar ice samples. Therefore, the DOC fraction promises even better suitability for dating thanks to its by a factor of 5 to 10 higher concentrations. Nevertheless, a straightforward analysis of DOC is hampered by its vulnerability to contamination. DOC consists in large part of mono- and dicarboxylic acids - compounds that can easily be taken up from the surrounding gas phase during sample preparation or which ...
author2 Schwikowski, Margit
format Doctoral or Postdoctoral Thesis
author Schindler, Johannes
author_facet Schindler, Johannes
author_sort Schindler, Johannes
title An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
title_short An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
title_full An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
title_fullStr An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
title_full_unstemmed An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice
title_sort extraction system for radiocarbon microanalysis of dissolved organic carbon in glacier ice
publishDate 2017
url https://boris.unibe.ch/99695/1/17schindler_j.pdf
https://boris.unibe.ch/99695/
genre ice core
genre_facet ice core
op_source Schindler, Johannes (2017). An Extraction System for Radiocarbon Microanalysis of Dissolved Organic Carbon in Glacier Ice. (Dissertation, Universität Bern, Philosophisch-naturwissenschaftliche Fakultät, Departement für Chemie und Biochemie)
op_relation https://boris.unibe.ch/99695/
op_rights info:eu-repo/semantics/openAccess
_version_ 1774718667857068032