An empirical method for absolute calibration of coccolith thickness

As major calcifiers in the open ocean, coccolithophores play a key role in the marine carbon cycle. Because they may be sensitive to changing CO2 and ocean acidification, there is significant interest in quantifying past and present variations in their cellular calcification by quantifying the thick...

Full description

Bibliographic Details
Main Authors: González-Lemos, Saúl, Guitián, José, Fuertes, Miguel-Ángel, Flores, José-Abel, Stoll, Heather M.
Format: Report
Language:English
Published: Copernicus 2017
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/233866
https://doi.org/10.3929/ethz-b-000233866
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/233866
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/233866 2023-05-15T17:51:29+02:00 An empirical method for absolute calibration of coccolith thickness González-Lemos, Saúl Guitián, José Fuertes, Miguel-Ángel Flores, José-Abel Stoll, Heather M. 2017-08-01 application/application/pdf https://hdl.handle.net/20.500.11850/233866 https://doi.org/10.3929/ethz-b-000233866 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-2017-249 http://hdl.handle.net/20.500.11850/233866 doi:10.3929/ethz-b-000233866 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International CC-BY Biogeosciences Discussions info:eu-repo/semantics/workingPaper 2017 ftethz https://doi.org/20.500.11850/233866 https://doi.org/10.3929/ethz-b-000233866 https://doi.org/10.5194/bg-2017-249 2023-02-13T01:05:17Z As major calcifiers in the open ocean, coccolithophores play a key role in the marine carbon cycle. Because they may be sensitive to changing CO2 and ocean acidification, there is significant interest in quantifying past and present variations in their cellular calcification by quantifying the thickness of the coccoliths or calcite plates that cover their cells. Polarized light microscopy has emerged as a key tool for quantifying the thickness of these calcite plates, but the reproducibility and accuracy of such determinations has been limited by the absence of suitable calibration materials in the thickness range of coccoliths (0–4 microns). Here, we describe the fabrication of a calcite wedge with a constant slope over 15 this thickness range, and the independent determination of calcite thickness along the wedge profile. We show how the calcite wedge provides more robust calibrations in the 0 to 1.55 μm range than previous approaches using rhabdoliths. We show the particular advantages of the calcite wedge approach for developing equations to relate thickness to the interference colors that arise in calcite in the thickness range between 1.55 and 4 μm. The calcite wedge approach can be applied to develop equations relevant to the particular light spectra and intensity of any polarized light microscope system and could significantly improve within and inter-laboratory data comparability. ISSN:1810-6277 ISSN:1810-6285 Report Ocean acidification ETH Zürich Research Collection
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
description As major calcifiers in the open ocean, coccolithophores play a key role in the marine carbon cycle. Because they may be sensitive to changing CO2 and ocean acidification, there is significant interest in quantifying past and present variations in their cellular calcification by quantifying the thickness of the coccoliths or calcite plates that cover their cells. Polarized light microscopy has emerged as a key tool for quantifying the thickness of these calcite plates, but the reproducibility and accuracy of such determinations has been limited by the absence of suitable calibration materials in the thickness range of coccoliths (0–4 microns). Here, we describe the fabrication of a calcite wedge with a constant slope over 15 this thickness range, and the independent determination of calcite thickness along the wedge profile. We show how the calcite wedge provides more robust calibrations in the 0 to 1.55 μm range than previous approaches using rhabdoliths. We show the particular advantages of the calcite wedge approach for developing equations to relate thickness to the interference colors that arise in calcite in the thickness range between 1.55 and 4 μm. The calcite wedge approach can be applied to develop equations relevant to the particular light spectra and intensity of any polarized light microscope system and could significantly improve within and inter-laboratory data comparability. ISSN:1810-6277 ISSN:1810-6285
format Report
author González-Lemos, Saúl
Guitián, José
Fuertes, Miguel-Ángel
Flores, José-Abel
Stoll, Heather M.
spellingShingle González-Lemos, Saúl
Guitián, José
Fuertes, Miguel-Ángel
Flores, José-Abel
Stoll, Heather M.
An empirical method for absolute calibration of coccolith thickness
author_facet González-Lemos, Saúl
Guitián, José
Fuertes, Miguel-Ángel
Flores, José-Abel
Stoll, Heather M.
author_sort González-Lemos, Saúl
title An empirical method for absolute calibration of coccolith thickness
title_short An empirical method for absolute calibration of coccolith thickness
title_full An empirical method for absolute calibration of coccolith thickness
title_fullStr An empirical method for absolute calibration of coccolith thickness
title_full_unstemmed An empirical method for absolute calibration of coccolith thickness
title_sort empirical method for absolute calibration of coccolith thickness
publisher Copernicus
publishDate 2017
url https://hdl.handle.net/20.500.11850/233866
https://doi.org/10.3929/ethz-b-000233866
genre Ocean acidification
genre_facet Ocean acidification
op_source Biogeosciences Discussions
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-2017-249
http://hdl.handle.net/20.500.11850/233866
doi:10.3929/ethz-b-000233866
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_rightsnorm CC-BY
op_doi https://doi.org/20.500.11850/233866
https://doi.org/10.3929/ethz-b-000233866
https://doi.org/10.5194/bg-2017-249
_version_ 1766158639134932992