Total water column analysis shows the importance of a single species in subsurface chlorophyll maximum thin layers in stratified waters
Total water column analysis shows the importance of a single species in subsurface chlorophyll maximum thin layers in stratified waters
Marine phytoplankton form the base of marine food webs and are the driving force of the marine carbon cycle, so understanding
the dynamics of their blooms is critical. While near-surface marine productivity (<10 m water depths) is extensively documented,
that of the subsurface is less well characterised. Increasing evidence of the importance of subsurface chlorophyll maxima (SCM) and
climatically driven increases in stratification of surface waters that promote SCM development call for improved sampling of the
subsurface. To address this, we targeted the summer stratified waters of the Western English Channel, part of the NW European
shelf seas, where SCM are commonly developed. In situ holography was applied to undertake the highest ever resolution, total
water column, quantitative analysis of microplankton distribution, and demonstrated the importance of a SCM, collocated with the
thermocline, dominated by a single species, the dinoflagellate Ceratium fusus. This species was dominant in the SCM over a wide
area of the NW European shelf in the June/ July 2015 study period and comprised up to 85% of the SCM biomass. Analysis of
similarity and multivariate non-metric multidimensional scaling showed the phytoplankton community of the SCM to be statistically
distinct from those of the surface and deep waters. Holography also revealed a fine scale layering of taxa at different levels within
the SCM, likely reflecting ecological differences. Some taxa followed the peak abundance of C. fusus, while others reached maximum
abundances immediately below or above the C. fusus maximum, suggesting the possible operation of exclusion mechanisms.
Additionally, the detection of abundant aggregates located only within and beneath the SCM demonstrates the potential importance
of this deep production for the export of carbon to the sea floor. Some predictions of phytoplankton productivity propose a shift to
smaller cells in the more stratified oceans of the future resulting in declining production and export. Results presented here,
however, contribute to a growing body of evidence that suggests, on the contrary, that key species among the larger celled/
colonial, SCM-adapted diatoms and dinoflagellates may instead be selected in stratified conditions, driving increased production and
export.
shelf seas, in situ observations, holography, primary production, phytoplankton, dinoflagellate, subsurface chlorophyll maximum, thermocline
1-19
Barnett, Michelle
fc382e7c-545c-42af-b5b2-65656518109d
Kemp, Alan
131b479e-c2c4-47ae-abe1-ad968490960e
Nimmo-Smith, Alex
634a7334-d841-4680-aa0b-b2f8f5b9ed1b
Purdie, Duncan
18820b32-185a-467a-8019-01f245191cd8
14 January 2022
Barnett, Michelle
fc382e7c-545c-42af-b5b2-65656518109d
Kemp, Alan
131b479e-c2c4-47ae-abe1-ad968490960e
Nimmo-Smith, Alex
634a7334-d841-4680-aa0b-b2f8f5b9ed1b
Purdie, Duncan
18820b32-185a-467a-8019-01f245191cd8
Barnett, Michelle, Kemp, Alan, Nimmo-Smith, Alex and Purdie, Duncan
(2022)
Total water column analysis shows the importance of a single species in subsurface chlorophyll maximum thin layers in stratified waters.
Frontiers in Marine Science, .
(doi:10.3389/fmars.2021.733791).
Abstract
Marine phytoplankton form the base of marine food webs and are the driving force of the marine carbon cycle, so understanding
the dynamics of their blooms is critical. While near-surface marine productivity (<10 m water depths) is extensively documented,
that of the subsurface is less well characterised. Increasing evidence of the importance of subsurface chlorophyll maxima (SCM) and
climatically driven increases in stratification of surface waters that promote SCM development call for improved sampling of the
subsurface. To address this, we targeted the summer stratified waters of the Western English Channel, part of the NW European
shelf seas, where SCM are commonly developed. In situ holography was applied to undertake the highest ever resolution, total
water column, quantitative analysis of microplankton distribution, and demonstrated the importance of a SCM, collocated with the
thermocline, dominated by a single species, the dinoflagellate Ceratium fusus. This species was dominant in the SCM over a wide
area of the NW European shelf in the June/ July 2015 study period and comprised up to 85% of the SCM biomass. Analysis of
similarity and multivariate non-metric multidimensional scaling showed the phytoplankton community of the SCM to be statistically
distinct from those of the surface and deep waters. Holography also revealed a fine scale layering of taxa at different levels within
the SCM, likely reflecting ecological differences. Some taxa followed the peak abundance of C. fusus, while others reached maximum
abundances immediately below or above the C. fusus maximum, suggesting the possible operation of exclusion mechanisms.
Additionally, the detection of abundant aggregates located only within and beneath the SCM demonstrates the potential importance
of this deep production for the export of carbon to the sea floor. Some predictions of phytoplankton productivity propose a shift to
smaller cells in the more stratified oceans of the future resulting in declining production and export. Results presented here,
however, contribute to a growing body of evidence that suggests, on the contrary, that key species among the larger celled/
colonial, SCM-adapted diatoms and dinoflagellates may instead be selected in stratified conditions, driving increased production and
export.
Other
733799_Manuscript (5)
More information
Accepted/In Press date: 17 December 2021
Published date: 14 January 2022
Keywords:
shelf seas, in situ observations, holography, primary production, phytoplankton, dinoflagellate, subsurface chlorophyll maximum, thermocline
Identifiers
Local EPrints ID: 453189
URI: http://eprints.soton.ac.uk/id/eprint/453189
ISSN: 2296-7745
PURE UUID: bf234ca1-931b-42e9-b797-1fa531804541
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Date deposited: 10 Jan 2022 18:03
Last modified: 17 Mar 2024 02:32
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Author:
Michelle Barnett
Author:
Alex Nimmo-Smith
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