The biogeochemical role of Coccolithus pelagicus

Coccolithophores are a biogeochemically important group of phytoplankton, responsible for around half of oceanic carbonate production through the formation of calcite coccoliths. Globally distributed, Emiliania huxleyi is generally perceived to be the key calcite producer, yet it has a relatively lo...

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Main Author: Daniels, Chris James
Format: Thesis
Language:English
Published: 2015
Subjects:
Online Access:https://eprints.soton.ac.uk/381144/
https://eprints.soton.ac.uk/381144/1/Daniels%252C%2520Chris_PhD_Thesis.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:381144 2023-07-30T04:02:04+02:00 The biogeochemical role of Coccolithus pelagicus Daniels, Chris James 2015-07-30 text https://eprints.soton.ac.uk/381144/ https://eprints.soton.ac.uk/381144/1/Daniels%252C%2520Chris_PhD_Thesis.pdf en English eng https://eprints.soton.ac.uk/381144/1/Daniels%252C%2520Chris_PhD_Thesis.pdf Daniels, Chris James (2015) The biogeochemical role of Coccolithus pelagicus. University of Southampton, Ocean & Earth Science, Doctoral Thesis, 173pp. Thesis NonPeerReviewed 2015 ftsouthampton 2023-07-09T22:01:23Z Coccolithophores are a biogeochemically important group of phytoplankton, responsible for around half of oceanic carbonate production through the formation of calcite coccoliths. Globally distributed, Emiliania huxleyi is generally perceived to be the key calcite producer, yet it has a relatively low cellular calcite content (~ 0.4 – 0.7 pmol C cell-1) compared to heavily calcified species such as Coccolithus pelagicus (~ 15 – 21 pmol C cell-1). This study set out to test the central hypothesis that C. pelagicus has a significant biogeochemical role, dominating calcite production within mixed communities in the North Atlantic. Cultures of Coccolithus species (C. pelagicus, C. braarudii) and E. huxleyi were grown in parallel to examine relative growth rates, and relative calcite production was modelled. While E. huxleyi grew faster than C. pelagicus, it was estimated that at the average relative growth rate observed, C. pelagicus calcified at a rate equivalent to 34 cells of E. huxleyi. This was compared to field samples of abundances from the North Atlantic, where C. pelagicus was found to be the major calcite producer in 69 % of the samples. At two sites in the North Atlantic (Iceland Basin, Norwegian Sea), repeat samples were collected during the early stages of the spring bloom to examine phytoplankton community dynamics and the role of coccolithophores. The two sites had contrasting communities with diatoms dominant in the Iceland Basin, but absent in the Norwegian Basin. The coccolithophore community was generally similar, with E. huxleyi dominating abundance and C. pelagicus dominating coccolithophore calcite. In situ growth rates found that C. pelagicus grew faster than E. huxleyi. In the Arctic and North Atlantic, species-specific calcite production was determined from measurements of calcite production and community composition. The results of this study indicated that C. pelagicus dominated calcite production despite forming only a small fraction (< 2 %) of the community. In the synthesis, the ... Thesis Arctic Iceland North Atlantic Norwegian Sea Phytoplankton University of Southampton: e-Prints Soton Arctic Norwegian Sea
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Coccolithophores are a biogeochemically important group of phytoplankton, responsible for around half of oceanic carbonate production through the formation of calcite coccoliths. Globally distributed, Emiliania huxleyi is generally perceived to be the key calcite producer, yet it has a relatively low cellular calcite content (~ 0.4 – 0.7 pmol C cell-1) compared to heavily calcified species such as Coccolithus pelagicus (~ 15 – 21 pmol C cell-1). This study set out to test the central hypothesis that C. pelagicus has a significant biogeochemical role, dominating calcite production within mixed communities in the North Atlantic. Cultures of Coccolithus species (C. pelagicus, C. braarudii) and E. huxleyi were grown in parallel to examine relative growth rates, and relative calcite production was modelled. While E. huxleyi grew faster than C. pelagicus, it was estimated that at the average relative growth rate observed, C. pelagicus calcified at a rate equivalent to 34 cells of E. huxleyi. This was compared to field samples of abundances from the North Atlantic, where C. pelagicus was found to be the major calcite producer in 69 % of the samples. At two sites in the North Atlantic (Iceland Basin, Norwegian Sea), repeat samples were collected during the early stages of the spring bloom to examine phytoplankton community dynamics and the role of coccolithophores. The two sites had contrasting communities with diatoms dominant in the Iceland Basin, but absent in the Norwegian Basin. The coccolithophore community was generally similar, with E. huxleyi dominating abundance and C. pelagicus dominating coccolithophore calcite. In situ growth rates found that C. pelagicus grew faster than E. huxleyi. In the Arctic and North Atlantic, species-specific calcite production was determined from measurements of calcite production and community composition. The results of this study indicated that C. pelagicus dominated calcite production despite forming only a small fraction (< 2 %) of the community. In the synthesis, the ...
format Thesis
author Daniels, Chris James
spellingShingle Daniels, Chris James
The biogeochemical role of Coccolithus pelagicus
author_facet Daniels, Chris James
author_sort Daniels, Chris James
title The biogeochemical role of Coccolithus pelagicus
title_short The biogeochemical role of Coccolithus pelagicus
title_full The biogeochemical role of Coccolithus pelagicus
title_fullStr The biogeochemical role of Coccolithus pelagicus
title_full_unstemmed The biogeochemical role of Coccolithus pelagicus
title_sort biogeochemical role of coccolithus pelagicus
publishDate 2015
url https://eprints.soton.ac.uk/381144/
https://eprints.soton.ac.uk/381144/1/Daniels%252C%2520Chris_PhD_Thesis.pdf
geographic Arctic
Norwegian Sea
geographic_facet Arctic
Norwegian Sea
genre Arctic
Iceland
North Atlantic
Norwegian Sea
Phytoplankton
genre_facet Arctic
Iceland
North Atlantic
Norwegian Sea
Phytoplankton
op_relation https://eprints.soton.ac.uk/381144/1/Daniels%252C%2520Chris_PhD_Thesis.pdf
Daniels, Chris James (2015) The biogeochemical role of Coccolithus pelagicus. University of Southampton, Ocean & Earth Science, Doctoral Thesis, 173pp.
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