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Ocean-scale modelling of the distribution, abundance, and seasonal dynamics of the copepod Calanus finmarchicus

Ocean-scale modelling of the distribution, abundance, and seasonal dynamics of the copepod Calanus finmarchicus
Ocean-scale modelling of the distribution, abundance, and seasonal dynamics of the copepod Calanus finmarchicus
The copepod Calanus finmarchicus is widely distributed over the sub-polar Atlantic and dominates the mesozooplanktonic biomass in that region. Despite this, all previous C. finmarchicus population modelling studies have been spatially and temporally limited. In this paper we present results from a fully stage-resolved model in a domain spanning the entire geographic range of the species (30 to 80°N and 80°W to 90° E. The model was driven by temperature and transport from the Ocean Circulation and Climate Advanced Modelling project (OCCAM) and phytoplankton food derived from satellite (SeaWiFS) sea-surface colour observations. The resulting quasi-stationary yearly cycle was assessed against seasonally resolved maps of continuous plankton recorder observations, winter cruise data on the distribution of diapausers, and time series from locations distributed over the North Atlantic. The model’s high computational efficiency permitted its free parameters to be selected to yield a good correspondence with the field data. We were also able to explore the effects of changing the assumptions regarding diapause and mortality. By falsifying alternative models we conclude that (1) a fixed fraction of each surface generation enters diapause, (2) overwintering individuals enter diapause at the end of the fifth copepodite stage, and (3) mortality is an increasing function of temperature. Finally, we demonstrate that the demographic impact of transport is limited, except in shelf seas and at the edges of the distribution; nevertheless, there is a very high level of population connectivity over the whole domain.
Calanus finmarchicus, structured population model, diapause, temperature dependent mortality, CPR, OCCAM, SeaWiFS
0171-8630
173-192
Speirs, D.C.
138307ca-e563-4cb4-a4d5-bd6fee8c9fec
Gurney, W.S.C.
4db9bcd5-8ccc-40ca-9dea-9aa54197ceea
Heath, M.R.
4ecd8835-b7c4-42ad-a49d-481b829cb217
Horbelt, W.
04b45a73-e8b3-4c03-85f4-6f88793f5e0a
Wood, S.N.
9e1eb8d9-b794-409c-8604-40f3dfdfbb05
de Cuevas, B.A.
01cc697c-2832-4de6-87bf-bf9f16c1f906
Speirs, D.C.
138307ca-e563-4cb4-a4d5-bd6fee8c9fec
Gurney, W.S.C.
4db9bcd5-8ccc-40ca-9dea-9aa54197ceea
Heath, M.R.
4ecd8835-b7c4-42ad-a49d-481b829cb217
Horbelt, W.
04b45a73-e8b3-4c03-85f4-6f88793f5e0a
Wood, S.N.
9e1eb8d9-b794-409c-8604-40f3dfdfbb05
de Cuevas, B.A.
01cc697c-2832-4de6-87bf-bf9f16c1f906

Speirs, D.C., Gurney, W.S.C., Heath, M.R., Horbelt, W., Wood, S.N. and de Cuevas, B.A. (2006) Ocean-scale modelling of the distribution, abundance, and seasonal dynamics of the copepod Calanus finmarchicus. Marine Ecology Progress Series, 313, 173-192.

Record type: Article

Abstract

The copepod Calanus finmarchicus is widely distributed over the sub-polar Atlantic and dominates the mesozooplanktonic biomass in that region. Despite this, all previous C. finmarchicus population modelling studies have been spatially and temporally limited. In this paper we present results from a fully stage-resolved model in a domain spanning the entire geographic range of the species (30 to 80°N and 80°W to 90° E. The model was driven by temperature and transport from the Ocean Circulation and Climate Advanced Modelling project (OCCAM) and phytoplankton food derived from satellite (SeaWiFS) sea-surface colour observations. The resulting quasi-stationary yearly cycle was assessed against seasonally resolved maps of continuous plankton recorder observations, winter cruise data on the distribution of diapausers, and time series from locations distributed over the North Atlantic. The model’s high computational efficiency permitted its free parameters to be selected to yield a good correspondence with the field data. We were also able to explore the effects of changing the assumptions regarding diapause and mortality. By falsifying alternative models we conclude that (1) a fixed fraction of each surface generation enters diapause, (2) overwintering individuals enter diapause at the end of the fifth copepodite stage, and (3) mortality is an increasing function of temperature. Finally, we demonstrate that the demographic impact of transport is limited, except in shelf seas and at the edges of the distribution; nevertheless, there is a very high level of population connectivity over the whole domain.

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More information

Published date: 2006
Keywords: Calanus finmarchicus, structured population model, diapause, temperature dependent mortality, CPR, OCCAM, SeaWiFS

Identifiers

Local EPrints ID: 44013
URI: http://eprints.soton.ac.uk/id/eprint/44013
ISSN: 0171-8630
PURE UUID: 0df85cb4-a934-4745-923e-9513773b118d

Catalogue record

Date deposited: 06 Feb 2007
Last modified: 08 Jan 2022 15:57

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Contributors

Author: D.C. Speirs
Author: W.S.C. Gurney
Author: M.R. Heath
Author: W. Horbelt
Author: S.N. Wood
Author: B.A. de Cuevas

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