A quantitative comparison of microfossil extraction methods from ice cores

Microfossil records from ice archives allow vegetation, fire and land-use activity reconstructions on broad spatial scales. Samples typically contain low microfossil concentrations. Therefore, large ice volumes are often needed for palynology. Hence, it is crucial to extract maximum microfossil numb...

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Published in:Journal of Glaciology
Main Authors: Brugger, Sandra O., Gobet, E., Schanz, F. R., Heiri, O., Schwoerer, C., Sigl, M., Schwikowski, M., Tinner, W.
Format: Article in Journal/Newspaper
Language:unknown
Published: CAMBRIDGE UNIV PRESS 2018
Subjects:
Online Access:https://edoc.unibas.ch/67169/
https://doi.org/10.1017/jog.2018.31
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spelling ftunivbasel:oai:edoc.unibas.ch:67169 2023-05-15T16:57:38+02:00 A quantitative comparison of microfossil extraction methods from ice cores Brugger, Sandra O. Gobet, E. Schanz, F. R. Heiri, O. Schwoerer, C. Sigl, M. Schwikowski, M. Tinner, W. 2018 https://edoc.unibas.ch/67169/ https://doi.org/10.1017/jog.2018.31 unknown CAMBRIDGE UNIV PRESS Brugger, Sandra O. and Gobet, E. and Schanz, F. R. and Heiri, O. and Schwoerer, C. and Sigl, M. and Schwikowski, M. and Tinner, W. (2018) A quantitative comparison of microfossil extraction methods from ice cores. JOURNAL OF GLACIOLOGY, 64 (245). pp. 432-442. doi:10.1017/jog.2018.31 info:isi/000434777300008 urn:ISSN:0022-1430 info:eu-repo/semantics/closedAccess Article PeerReviewed 2018 ftunivbasel https://doi.org/10.1017/jog.2018.31 2023-03-05T07:20:32Z Microfossil records from ice archives allow vegetation, fire and land-use activity reconstructions on broad spatial scales. Samples typically contain low microfossil concentrations. Therefore, large ice volumes are often needed for palynology. Hence, it is crucial to extract maximum microfossil numbers through appropriate physical-chemical treatments. We compare six methods covering the main water reduction procedures: evaporation, filtration and centrifugation with snow samples. Adding a known number of Lycopodium marker spores prior to sample treatment and a second marker (Eucalyptus) after laboratory processing allows a quantitative microfossil loss assessment during pollen extraction. We applied the best-performing method (average loss of 22%) to high-alpine firn cores from Colle Gnifetti glacier for validation with a natural archive containing extremely low microfossil concentrations. We conclude that samples processed with different microfossil extraction protocols may give different results for pollen concentrations, percentages and ratios between different pollen types, especially if vesiculate conifer pollen is an important pollen assemblage component. We recommend a new evaporation-based method which delivers the smallest and least variable losses among the tested approaches. Since microfossil losses are inevitable during laboratory procedure, adding markers prior to sample processing is mandatory to achieve reliable microfossil concentration and influx estimates. Article in Journal/Newspaper Journal of Glaciology University of Basel: edoc Journal of Glaciology 64 245 432 442
institution Open Polar
collection University of Basel: edoc
op_collection_id ftunivbasel
language unknown
description Microfossil records from ice archives allow vegetation, fire and land-use activity reconstructions on broad spatial scales. Samples typically contain low microfossil concentrations. Therefore, large ice volumes are often needed for palynology. Hence, it is crucial to extract maximum microfossil numbers through appropriate physical-chemical treatments. We compare six methods covering the main water reduction procedures: evaporation, filtration and centrifugation with snow samples. Adding a known number of Lycopodium marker spores prior to sample treatment and a second marker (Eucalyptus) after laboratory processing allows a quantitative microfossil loss assessment during pollen extraction. We applied the best-performing method (average loss of 22%) to high-alpine firn cores from Colle Gnifetti glacier for validation with a natural archive containing extremely low microfossil concentrations. We conclude that samples processed with different microfossil extraction protocols may give different results for pollen concentrations, percentages and ratios between different pollen types, especially if vesiculate conifer pollen is an important pollen assemblage component. We recommend a new evaporation-based method which delivers the smallest and least variable losses among the tested approaches. Since microfossil losses are inevitable during laboratory procedure, adding markers prior to sample processing is mandatory to achieve reliable microfossil concentration and influx estimates.
format Article in Journal/Newspaper
author Brugger, Sandra O.
Gobet, E.
Schanz, F. R.
Heiri, O.
Schwoerer, C.
Sigl, M.
Schwikowski, M.
Tinner, W.
spellingShingle Brugger, Sandra O.
Gobet, E.
Schanz, F. R.
Heiri, O.
Schwoerer, C.
Sigl, M.
Schwikowski, M.
Tinner, W.
A quantitative comparison of microfossil extraction methods from ice cores
author_facet Brugger, Sandra O.
Gobet, E.
Schanz, F. R.
Heiri, O.
Schwoerer, C.
Sigl, M.
Schwikowski, M.
Tinner, W.
author_sort Brugger, Sandra O.
title A quantitative comparison of microfossil extraction methods from ice cores
title_short A quantitative comparison of microfossil extraction methods from ice cores
title_full A quantitative comparison of microfossil extraction methods from ice cores
title_fullStr A quantitative comparison of microfossil extraction methods from ice cores
title_full_unstemmed A quantitative comparison of microfossil extraction methods from ice cores
title_sort quantitative comparison of microfossil extraction methods from ice cores
publisher CAMBRIDGE UNIV PRESS
publishDate 2018
url https://edoc.unibas.ch/67169/
https://doi.org/10.1017/jog.2018.31
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation Brugger, Sandra O. and Gobet, E. and Schanz, F. R. and Heiri, O. and Schwoerer, C. and Sigl, M. and Schwikowski, M. and Tinner, W. (2018) A quantitative comparison of microfossil extraction methods from ice cores. JOURNAL OF GLACIOLOGY, 64 (245). pp. 432-442.
doi:10.1017/jog.2018.31
info:isi/000434777300008
urn:ISSN:0022-1430
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1017/jog.2018.31
container_title Journal of Glaciology
container_volume 64
container_issue 245
container_start_page 432
op_container_end_page 442
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