Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.

Fish populations are linked to ocean biogeochemistry by their reliance on primary production for food, and dissolved oxygen to breathe. It is also possible that marine fish modify biogeochemical dynamics, as do freshwater fish, through top-down trophic cascades, but there has been relatively little...

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Main Authors: Lucas Kavanagh, Eric Galbraith
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2018-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC6070179?pdf=render
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spelling doaj-657053ba55db4ffab2a06d6111d8b97c2020-11-24T21:09:42ZengPublic Library of Science (PLoS)PLoS ONE1932-62032018-01-01138e019942010.1371/journal.pone.0199420Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.Lucas KavanaghEric GalbraithFish populations are linked to ocean biogeochemistry by their reliance on primary production for food, and dissolved oxygen to breathe. It is also possible that marine fish modify biogeochemical dynamics, as do freshwater fish, through top-down trophic cascades, but there has been relatively little consideration of this possibility. This lack of consideration may reflect a lack of importance; alternatively, it may simply reflect the lack of appropriate observations with which to constrain such relationships. Here, we draw attention to the potential use of marine sediments as long-term simultaneous monitors of both fish abundance and marine biogeochemical dynamics. We compile published sediment proxy records of fish abundance from the west coasts of the Americas, and compare them with biogeochemical proxy measurements made at the same sites. Despite the challenges of using sediment records and the potential convolution of ecological and climatic signals, we find a small number of statistically significant relationships between fish debris and biogeochemical variables, at least some of which are likely to reflect causal relationships. Considering TOC, the most commonly-measured biogeochemical variable, some positive correlations with fish abundance are found, consistent with bottom-up control of fish abundance by primary production, or a planktivore-herbivore-phytoplankton trophic cascade. Negative correlations are also found, which could reflect sedimentary processes, the influence of upwelling-driven oxygen and nutrient dynamics on primary production and fish populations, and/or impacts of fish stocks on carbon fluxes by altering the recycling of carbon within the water column. Although the number of available measurements is too small to draw strong conclusions, the results point to plausible cases of bottom-up forcing, trophic cascades, and influence of dissolved oxygen concentrations on fish habitat.http://europepmc.org/articles/PMC6070179?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Lucas Kavanagh
Eric Galbraith
spellingShingle Lucas Kavanagh
Eric Galbraith
Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
PLoS ONE
author_facet Lucas Kavanagh
Eric Galbraith
author_sort Lucas Kavanagh
title Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
title_short Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
title_full Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
title_fullStr Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
title_full_unstemmed Links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
title_sort links between fish abundance and ocean biogeochemistry as recorded in marine sediments.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2018-01-01
description Fish populations are linked to ocean biogeochemistry by their reliance on primary production for food, and dissolved oxygen to breathe. It is also possible that marine fish modify biogeochemical dynamics, as do freshwater fish, through top-down trophic cascades, but there has been relatively little consideration of this possibility. This lack of consideration may reflect a lack of importance; alternatively, it may simply reflect the lack of appropriate observations with which to constrain such relationships. Here, we draw attention to the potential use of marine sediments as long-term simultaneous monitors of both fish abundance and marine biogeochemical dynamics. We compile published sediment proxy records of fish abundance from the west coasts of the Americas, and compare them with biogeochemical proxy measurements made at the same sites. Despite the challenges of using sediment records and the potential convolution of ecological and climatic signals, we find a small number of statistically significant relationships between fish debris and biogeochemical variables, at least some of which are likely to reflect causal relationships. Considering TOC, the most commonly-measured biogeochemical variable, some positive correlations with fish abundance are found, consistent with bottom-up control of fish abundance by primary production, or a planktivore-herbivore-phytoplankton trophic cascade. Negative correlations are also found, which could reflect sedimentary processes, the influence of upwelling-driven oxygen and nutrient dynamics on primary production and fish populations, and/or impacts of fish stocks on carbon fluxes by altering the recycling of carbon within the water column. Although the number of available measurements is too small to draw strong conclusions, the results point to plausible cases of bottom-up forcing, trophic cascades, and influence of dissolved oxygen concentrations on fish habitat.
url http://europepmc.org/articles/PMC6070179?pdf=render
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