A novel approach reveals high zooplankton standing stock deep in the sea

In a changing ocean there is a critical need to understand global biogeochemical cycling, particularly regarding carbon. We have made strides in understanding upper ocean dynamics, but the deep ocean interior (> 1000 m) is still largely unknown, despite representing the overwhelming major...

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Main Authors: A. Vereshchaka, G. Abyzova, A. Lunina, E. Musaeva, T. Sutton
Format: Article
Language:English
Published: Copernicus Publications 2016-11-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/13/6261/2016/bg-13-6261-2016.pdf
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spelling doaj-ca07bf2c7eda496fb6b145e7f5c775832020-11-25T01:05:56ZengCopernicus PublicationsBiogeosciences1726-41701726-41892016-11-01136261627110.5194/bg-13-6261-2016A novel approach reveals high zooplankton standing stock deep in the seaA. Vereshchaka0G. Abyzova1A. Lunina2E. Musaeva3T. Sutton4Institute of Oceanology, Russian Academy of Sciences, Nakhimov Pr. 36, Moscow, 117997 RussiaInstitute of Oceanology, Russian Academy of Sciences, Nakhimov Pr. 36, Moscow, 117997 RussiaInstitute of Oceanology, Russian Academy of Sciences, Nakhimov Pr. 36, Moscow, 117997 RussiaInstitute of Oceanology, Russian Academy of Sciences, Nakhimov Pr. 36, Moscow, 117997 RussiaHalmos College of Natural Sciences and Oceanography, Nova Southeastern University, Dania Beach, FL 33004, USAIn a changing ocean there is a critical need to understand global biogeochemical cycling, particularly regarding carbon. We have made strides in understanding upper ocean dynamics, but the deep ocean interior (> 1000 m) is still largely unknown, despite representing the overwhelming majority of Earth's biosphere. Here we present a method for estimating deep-pelagic zooplankton biomass on an ocean-basin scale. We have made several new discoveries about the Atlantic, which likely apply to the world ocean. First, multivariate analysis showed that depth and Chl were the basic factors affecting the wet biomass of the main plankton groups. Wet biomass of all major groups was significantly correlated with Chl. Second, zooplankton biomass in the upper bathypelagic domain is higher than expected. Third, the majority of this biomass comprises macroplanktonic shrimps, which have been historically underestimated. These findings, coupled with recent findings of increased global deep-pelagic fish biomass, suggest that the contribution of the deep-ocean pelagic fauna for biogeochemical cycles may be more important than previously thought.https://www.biogeosciences.net/13/6261/2016/bg-13-6261-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Vereshchaka
G. Abyzova
A. Lunina
E. Musaeva
T. Sutton
spellingShingle A. Vereshchaka
G. Abyzova
A. Lunina
E. Musaeva
T. Sutton
A novel approach reveals high zooplankton standing stock deep in the sea
Biogeosciences
author_facet A. Vereshchaka
G. Abyzova
A. Lunina
E. Musaeva
T. Sutton
author_sort A. Vereshchaka
title A novel approach reveals high zooplankton standing stock deep in the sea
title_short A novel approach reveals high zooplankton standing stock deep in the sea
title_full A novel approach reveals high zooplankton standing stock deep in the sea
title_fullStr A novel approach reveals high zooplankton standing stock deep in the sea
title_full_unstemmed A novel approach reveals high zooplankton standing stock deep in the sea
title_sort novel approach reveals high zooplankton standing stock deep in the sea
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2016-11-01
description In a changing ocean there is a critical need to understand global biogeochemical cycling, particularly regarding carbon. We have made strides in understanding upper ocean dynamics, but the deep ocean interior (> 1000 m) is still largely unknown, despite representing the overwhelming majority of Earth's biosphere. Here we present a method for estimating deep-pelagic zooplankton biomass on an ocean-basin scale. We have made several new discoveries about the Atlantic, which likely apply to the world ocean. First, multivariate analysis showed that depth and Chl were the basic factors affecting the wet biomass of the main plankton groups. Wet biomass of all major groups was significantly correlated with Chl. Second, zooplankton biomass in the upper bathypelagic domain is higher than expected. Third, the majority of this biomass comprises macroplanktonic shrimps, which have been historically underestimated. These findings, coupled with recent findings of increased global deep-pelagic fish biomass, suggest that the contribution of the deep-ocean pelagic fauna for biogeochemical cycles may be more important than previously thought.
url https://www.biogeosciences.net/13/6261/2016/bg-13-6261-2016.pdf
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