Long‐term resilience in microcrustacean communities despite environmental changes

Abstract The ability of communities to withstand stress or maintain their species composition over extended periods of environmental changes is a matter of major concern. Here, we utilize a dataset where microcrustacean communities were related to water chemistry in 82 boreal‐alpine lakes over a 50‐...

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Main Authors: M. Eie, T. C. Jensen, B. Walseng, A. J. Eie, D. O. Hessen
Format: Article
Language:English
Published: Wiley 2021-07-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1002/ecs2.3676
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spelling doaj-7b7ddf73cc4546a28de16d3506eb79ee2021-07-29T10:34:35ZengWileyEcosphere2150-89252021-07-01127n/an/a10.1002/ecs2.3676Long‐term resilience in microcrustacean communities despite environmental changesM. Eie0T. C. Jensen1B. Walseng2A. J. Eie3D. O. Hessen4County Governor of Agder Box 788 Stoa Arendal 4809 NorwayNorwegian Institute for Nature Research Sognsveien 68 Oslo 0855 NorwayNorwegian Institute for Nature Research Sognsveien 68 Oslo 0855 NorwaySeljeveien 8 Ski 1406 NorwayDepartment of Biosciences and Centre for Biogeochemistry in the Anthropocene University of Oslo Box 1066Blindern Oslo 0316 NorwayAbstract The ability of communities to withstand stress or maintain their species composition over extended periods of environmental changes is a matter of major concern. Here, we utilize a dataset where microcrustacean communities were related to water chemistry in 82 boreal‐alpine lakes over a 50‐yr time span (1968 and 2016), with the same person involved in sampling both times ensuring identical sites and sampling protocols. Over this time span, there has been a 1–2°C increase in mean annual temperatures and prolonged growing seasons. Also, the strong changes in SO4 deposition and acidification, peaking in the early 1980s, followed by a recovery period, have caused not only an increase in pH but also a pronounced browning (elevated DOC) and reduced levels of Ca over the past three decades. Despite this, the microcrustacean diversity and community composition have remained remarkably stable, and this holds both for the species‐rich larger, boreal sites and the species‐poor alpine sites. While likely there are interannual fluctuations in species abundance, and perhaps species may also be missing for certain periods, a combination of local refugia, resting egg seed‐banks and a regional recolonization that may occur at the meta‐population level, aims at maintaining a strong stability in community composition.https://doi.org/10.1002/ecs2.3676browningcalciumlakesresiliencerichnesszooplankton
collection DOAJ
language English
format Article
sources DOAJ
author M. Eie
T. C. Jensen
B. Walseng
A. J. Eie
D. O. Hessen
spellingShingle M. Eie
T. C. Jensen
B. Walseng
A. J. Eie
D. O. Hessen
Long‐term resilience in microcrustacean communities despite environmental changes
Ecosphere
browning
calcium
lakes
resilience
richness
zooplankton
author_facet M. Eie
T. C. Jensen
B. Walseng
A. J. Eie
D. O. Hessen
author_sort M. Eie
title Long‐term resilience in microcrustacean communities despite environmental changes
title_short Long‐term resilience in microcrustacean communities despite environmental changes
title_full Long‐term resilience in microcrustacean communities despite environmental changes
title_fullStr Long‐term resilience in microcrustacean communities despite environmental changes
title_full_unstemmed Long‐term resilience in microcrustacean communities despite environmental changes
title_sort long‐term resilience in microcrustacean communities despite environmental changes
publisher Wiley
series Ecosphere
issn 2150-8925
publishDate 2021-07-01
description Abstract The ability of communities to withstand stress or maintain their species composition over extended periods of environmental changes is a matter of major concern. Here, we utilize a dataset where microcrustacean communities were related to water chemistry in 82 boreal‐alpine lakes over a 50‐yr time span (1968 and 2016), with the same person involved in sampling both times ensuring identical sites and sampling protocols. Over this time span, there has been a 1–2°C increase in mean annual temperatures and prolonged growing seasons. Also, the strong changes in SO4 deposition and acidification, peaking in the early 1980s, followed by a recovery period, have caused not only an increase in pH but also a pronounced browning (elevated DOC) and reduced levels of Ca over the past three decades. Despite this, the microcrustacean diversity and community composition have remained remarkably stable, and this holds both for the species‐rich larger, boreal sites and the species‐poor alpine sites. While likely there are interannual fluctuations in species abundance, and perhaps species may also be missing for certain periods, a combination of local refugia, resting egg seed‐banks and a regional recolonization that may occur at the meta‐population level, aims at maintaining a strong stability in community composition.
topic browning
calcium
lakes
resilience
richness
zooplankton
url https://doi.org/10.1002/ecs2.3676
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