Patchiness of phytoplankton and primary production in Liaodong Bay, China.

A comprehensive study of water quality, phytoplankton biomass, and photosynthetic rates in Liaodong Bay, China, during June and July of 2013 revealed two large patches of high biomass and production with dimensions on the order of 10 km. Nutrient concentrations were above growth-rate-saturating conc...

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Main Authors: Shaofeng Pei, Edward A Laws, Haibo Zhang, Siyuan Ye, Hongming Yuan, Haiyue Liu
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2017-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC5325570?pdf=render
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spelling doaj-5f23ff2d58944b60a631e6c8b9be4ac52020-11-25T00:08:53ZengPublic Library of Science (PLoS)PLoS ONE1932-62032017-01-01122e017306710.1371/journal.pone.0173067Patchiness of phytoplankton and primary production in Liaodong Bay, China.Shaofeng PeiEdward A LawsHaibo ZhangSiyuan YeHongming YuanHaiyue LiuA comprehensive study of water quality, phytoplankton biomass, and photosynthetic rates in Liaodong Bay, China, during June and July of 2013 revealed two large patches of high biomass and production with dimensions on the order of 10 km. Nutrient concentrations were above growth-rate-saturating concentrations throughout the bay, with the possible exception of phosphate at some stations. The presence of the patches therefore appeared to reflect the distribution of water temperature and variation of light penetration restricted by water turbidity. There was no patch of high phytoplankton biomass or production in a third, linear patch of water with characteristics suitable for rapid phytoplankton growth; the absence of a bloom in that patch likely reflected the fact that the width of the patch was less than the critical size required to overcome losses of phytoplankton to turbulent diffusion. The bottom waters of virtually all of the eastern half of the bay were below the depth of the mixed layer, and the lowest bottom water oxygen concentrations, 3-5 mg L-1, were found in that part of the bay. The water column in much of the remainder of the bay was within the mixed layer, and oxygen concentrations in both surface and bottom waters exceeded 5 mg L-1.http://europepmc.org/articles/PMC5325570?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Shaofeng Pei
Edward A Laws
Haibo Zhang
Siyuan Ye
Hongming Yuan
Haiyue Liu
spellingShingle Shaofeng Pei
Edward A Laws
Haibo Zhang
Siyuan Ye
Hongming Yuan
Haiyue Liu
Patchiness of phytoplankton and primary production in Liaodong Bay, China.
PLoS ONE
author_facet Shaofeng Pei
Edward A Laws
Haibo Zhang
Siyuan Ye
Hongming Yuan
Haiyue Liu
author_sort Shaofeng Pei
title Patchiness of phytoplankton and primary production in Liaodong Bay, China.
title_short Patchiness of phytoplankton and primary production in Liaodong Bay, China.
title_full Patchiness of phytoplankton and primary production in Liaodong Bay, China.
title_fullStr Patchiness of phytoplankton and primary production in Liaodong Bay, China.
title_full_unstemmed Patchiness of phytoplankton and primary production in Liaodong Bay, China.
title_sort patchiness of phytoplankton and primary production in liaodong bay, china.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2017-01-01
description A comprehensive study of water quality, phytoplankton biomass, and photosynthetic rates in Liaodong Bay, China, during June and July of 2013 revealed two large patches of high biomass and production with dimensions on the order of 10 km. Nutrient concentrations were above growth-rate-saturating concentrations throughout the bay, with the possible exception of phosphate at some stations. The presence of the patches therefore appeared to reflect the distribution of water temperature and variation of light penetration restricted by water turbidity. There was no patch of high phytoplankton biomass or production in a third, linear patch of water with characteristics suitable for rapid phytoplankton growth; the absence of a bloom in that patch likely reflected the fact that the width of the patch was less than the critical size required to overcome losses of phytoplankton to turbulent diffusion. The bottom waters of virtually all of the eastern half of the bay were below the depth of the mixed layer, and the lowest bottom water oxygen concentrations, 3-5 mg L-1, were found in that part of the bay. The water column in much of the remainder of the bay was within the mixed layer, and oxygen concentrations in both surface and bottom waters exceeded 5 mg L-1.
url http://europepmc.org/articles/PMC5325570?pdf=render
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