Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer

Current versions of plankton production models which allow variability in the vertical plane are based on very slender assumptions about vertical distributions of zooplankton. A late summer LHPR section across the N.E. Atlantic and some spring and early summer LHPR hauls at 59°N indicate some of the...

Full description

Bibliographic Details
Published in:Journal of Plankton Research
Main Authors: Longhurst, Alan, Williams, Robert
Format: Text
Language:English
Published: Oxford University Press 1979
Subjects:
Online Access:http://plankt.oxfordjournals.org/cgi/content/short/1/1/1
https://doi.org/10.1093/plankt/1.1.1
id fthighwire:oai:open-archive.highwire.org:plankt:1/1/1
record_format openpolar
spelling fthighwire:oai:open-archive.highwire.org:plankt:1/1/1 2023-05-15T17:35:01+02:00 Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer Longhurst, Alan Williams, Robert 1979-04-01 00:00:00.0 text/html http://plankt.oxfordjournals.org/cgi/content/short/1/1/1 https://doi.org/10.1093/plankt/1.1.1 en eng Oxford University Press http://plankt.oxfordjournals.org/cgi/content/short/1/1/1 http://dx.doi.org/10.1093/plankt/1.1.1 Copyright (C) 1979, Oxford University Press Articles TEXT 1979 fthighwire https://doi.org/10.1093/plankt/1.1.1 2015-02-28T22:08:52Z Current versions of plankton production models which allow variability in the vertical plane are based on very slender assumptions about vertical distributions of zooplankton. A late summer LHPR section across the N.E. Atlantic and some spring and early summer LHPR hauls at 59°N indicate some of the details of vertical distribution which seem to be important for model-formulation. It is suggested that a model which is designed to simulate vertical plankton structure in the North Atlantic should cause zooplankton to be distributed during the production period so as to satisfy the following criteria: 60–70% of the biomass must be of carnivores, and 25–75% of all biomass should come to be located within a discrete epiplankton layer within 40 d of the start of the seasonal production: this epiplankton should extend down to 3–4 times the depth of the mixed layer, with its lower limit near the base of the seasonal tbermocline; the epiplankton must extend deeper than the depth of negligible chlorophyll, and 3–4 times deeper than the chorophyll mnTimnm; maximum concentrations of filter-feeders should be located at aboout half the depth of the chlorophyll maximum, and the mmimnm of predators rather deeper; below the epiplankton, biomass should be rather constant down to 1,000 m, be about 15–30 times less abundant than the epiplankton, and should contain discrete layers of interzonal migrants. It is suggested, by reference to FLEX LHPR profiles, that there are important differences between the oceanic plankton and the copepod-dominated spring plankton in the North Sea, which will have important consequences for plankton modelling. Text North Atlantic HighWire Press (Stanford University) Journal of Plankton Research 1 1 1 28
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Longhurst, Alan
Williams, Robert
Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
topic_facet Articles
description Current versions of plankton production models which allow variability in the vertical plane are based on very slender assumptions about vertical distributions of zooplankton. A late summer LHPR section across the N.E. Atlantic and some spring and early summer LHPR hauls at 59°N indicate some of the details of vertical distribution which seem to be important for model-formulation. It is suggested that a model which is designed to simulate vertical plankton structure in the North Atlantic should cause zooplankton to be distributed during the production period so as to satisfy the following criteria: 60–70% of the biomass must be of carnivores, and 25–75% of all biomass should come to be located within a discrete epiplankton layer within 40 d of the start of the seasonal production: this epiplankton should extend down to 3–4 times the depth of the mixed layer, with its lower limit near the base of the seasonal tbermocline; the epiplankton must extend deeper than the depth of negligible chlorophyll, and 3–4 times deeper than the chorophyll mnTimnm; maximum concentrations of filter-feeders should be located at aboout half the depth of the chlorophyll maximum, and the mmimnm of predators rather deeper; below the epiplankton, biomass should be rather constant down to 1,000 m, be about 15–30 times less abundant than the epiplankton, and should contain discrete layers of interzonal migrants. It is suggested, by reference to FLEX LHPR profiles, that there are important differences between the oceanic plankton and the copepod-dominated spring plankton in the North Sea, which will have important consequences for plankton modelling.
format Text
author Longhurst, Alan
Williams, Robert
author_facet Longhurst, Alan
Williams, Robert
author_sort Longhurst, Alan
title Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
title_short Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
title_full Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
title_fullStr Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
title_full_unstemmed Materials for plankton modelling: Vertical distribution of Atlantic zooplankton in summer
title_sort materials for plankton modelling: vertical distribution of atlantic zooplankton in summer
publisher Oxford University Press
publishDate 1979
url http://plankt.oxfordjournals.org/cgi/content/short/1/1/1
https://doi.org/10.1093/plankt/1.1.1
genre North Atlantic
genre_facet North Atlantic
op_relation http://plankt.oxfordjournals.org/cgi/content/short/1/1/1
http://dx.doi.org/10.1093/plankt/1.1.1
op_rights Copyright (C) 1979, Oxford University Press
op_doi https://doi.org/10.1093/plankt/1.1.1
container_title Journal of Plankton Research
container_volume 1
container_issue 1
container_start_page 1
op_container_end_page 28
_version_ 1766134043860008960