An alternative method for correcting fluorescence quenching

Under high light intensity, phytoplankton protect their photosystems from bleaching through non-photochemical quenching processes. The consequence of this is suppression of fluorescence emission, which must be corrected when measuring in situ yield with fluorometers. We present data from the Souther...

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Published in:Ocean Science
Main Authors: L. Biermann, C. Guinet, M. Bester, A. Brierley, L. Boehme
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
geo
Online Access:https://doi.org/10.5194/os-11-83-2015
http://www.ocean-sci.net/11/83/2015/os-11-83-2015.pdf
https://doaj.org/article/de73be1d08094651abc76b4573a52dfc
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:de73be1d08094651abc76b4573a52dfc 2023-05-15T16:05:43+02:00 An alternative method for correcting fluorescence quenching L. Biermann C. Guinet M. Bester A. Brierley L. Boehme 2015-01-01 https://doi.org/10.5194/os-11-83-2015 http://www.ocean-sci.net/11/83/2015/os-11-83-2015.pdf https://doaj.org/article/de73be1d08094651abc76b4573a52dfc en eng Copernicus Publications 1812-0784 1812-0792 doi:10.5194/os-11-83-2015 http://www.ocean-sci.net/11/83/2015/os-11-83-2015.pdf https://doaj.org/article/de73be1d08094651abc76b4573a52dfc undefined Ocean Science, Vol 11, Iss 1, Pp 83-91 (2015) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/os-11-83-2015 2023-01-22T19:34:33Z Under high light intensity, phytoplankton protect their photosystems from bleaching through non-photochemical quenching processes. The consequence of this is suppression of fluorescence emission, which must be corrected when measuring in situ yield with fluorometers. We present data from the Southern Ocean, collected over five austral summers by 19 southern elephant seals tagged with fluorometers. Conventionally, fluorescence data collected during the day (quenched) were corrected using the limit of the mixed layer, assuming that phytoplankton are uniformly mixed from the surface to this depth. However, distinct deep fluorescence maxima were measured in approximately 30% of the night (unquenched) data. To account for the evidence that chlorophyll is not uniformly mixed in the upper layer, we propose correcting from the limit of the euphotic zone, defined as the depth at which photosynthetically available radiation is ~ 1% of the surface value. Mixed layer depth exceeded euphotic depth over 80% of the time. Under these conditions, quenching was corrected from the depth of the remotely derived euphotic zone Zeu, and compared with fluorescence corrected from the depth of the density-derived mixed layer. Deep fluorescence maxima were evident in only 10% of the day data when correcting from mixed layer depth. This was doubled to 21% when correcting from Zeu, more closely matching the unquenched (night) data. Furthermore, correcting from Zeu served to conserve non-uniform chlorophyll features found between the 1% light level and mixed layer depth. Article in Journal/Newspaper Elephant Seals Southern Elephant Seals Southern Ocean Unknown Austral Southern Ocean Ocean Science 11 1 83 91
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic envir
geo
spellingShingle envir
geo
L. Biermann
C. Guinet
M. Bester
A. Brierley
L. Boehme
An alternative method for correcting fluorescence quenching
topic_facet envir
geo
description Under high light intensity, phytoplankton protect their photosystems from bleaching through non-photochemical quenching processes. The consequence of this is suppression of fluorescence emission, which must be corrected when measuring in situ yield with fluorometers. We present data from the Southern Ocean, collected over five austral summers by 19 southern elephant seals tagged with fluorometers. Conventionally, fluorescence data collected during the day (quenched) were corrected using the limit of the mixed layer, assuming that phytoplankton are uniformly mixed from the surface to this depth. However, distinct deep fluorescence maxima were measured in approximately 30% of the night (unquenched) data. To account for the evidence that chlorophyll is not uniformly mixed in the upper layer, we propose correcting from the limit of the euphotic zone, defined as the depth at which photosynthetically available radiation is ~ 1% of the surface value. Mixed layer depth exceeded euphotic depth over 80% of the time. Under these conditions, quenching was corrected from the depth of the remotely derived euphotic zone Zeu, and compared with fluorescence corrected from the depth of the density-derived mixed layer. Deep fluorescence maxima were evident in only 10% of the day data when correcting from mixed layer depth. This was doubled to 21% when correcting from Zeu, more closely matching the unquenched (night) data. Furthermore, correcting from Zeu served to conserve non-uniform chlorophyll features found between the 1% light level and mixed layer depth.
format Article in Journal/Newspaper
author L. Biermann
C. Guinet
M. Bester
A. Brierley
L. Boehme
author_facet L. Biermann
C. Guinet
M. Bester
A. Brierley
L. Boehme
author_sort L. Biermann
title An alternative method for correcting fluorescence quenching
title_short An alternative method for correcting fluorescence quenching
title_full An alternative method for correcting fluorescence quenching
title_fullStr An alternative method for correcting fluorescence quenching
title_full_unstemmed An alternative method for correcting fluorescence quenching
title_sort alternative method for correcting fluorescence quenching
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/os-11-83-2015
http://www.ocean-sci.net/11/83/2015/os-11-83-2015.pdf
https://doaj.org/article/de73be1d08094651abc76b4573a52dfc
geographic Austral
Southern Ocean
geographic_facet Austral
Southern Ocean
genre Elephant Seals
Southern Elephant Seals
Southern Ocean
genre_facet Elephant Seals
Southern Elephant Seals
Southern Ocean
op_source Ocean Science, Vol 11, Iss 1, Pp 83-91 (2015)
op_relation 1812-0784
1812-0792
doi:10.5194/os-11-83-2015
http://www.ocean-sci.net/11/83/2015/os-11-83-2015.pdf
https://doaj.org/article/de73be1d08094651abc76b4573a52dfc
op_rights undefined
op_doi https://doi.org/10.5194/os-11-83-2015
container_title Ocean Science
container_volume 11
container_issue 1
container_start_page 83
op_container_end_page 91
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