Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?

That biodiversity declines with latitude is well known, but whether a metacommunity process is behind this gradient has received limited attention. We tested the hypothesis that dispersal limitation is progressively replaced by mass effects with increasing latitude, along with a series of related hy...

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Main Authors: Jonathan D. Tonkin, Russell G. Death, Timo Muotka, Anna Astorga, David A. Lytle
Format: Article
Language:English
Published: PeerJ Inc. 2018-05-01
Series:PeerJ
Subjects:
Online Access:https://peerj.com/articles/4898.pdf
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author Jonathan D. Tonkin
Russell G. Death
Timo Muotka
Anna Astorga
David A. Lytle
author_facet Jonathan D. Tonkin
Russell G. Death
Timo Muotka
Anna Astorga
David A. Lytle
author_sort Jonathan D. Tonkin
collection DOAJ
description That biodiversity declines with latitude is well known, but whether a metacommunity process is behind this gradient has received limited attention. We tested the hypothesis that dispersal limitation is progressively replaced by mass effects with increasing latitude, along with a series of related hypotheses. We explored these hypotheses by examining metacommunity structure in stream invertebrate metacommunities spanning the length of New Zealand’s two largest islands (∼1,300 km), further disentangling the role of dispersal by deconstructing assemblages into strong and weak dispersers. Given the highly dynamic nature of New Zealand streams, our alternative hypothesis was that these systems are so unpredictable (at different stages of post-flood succession) that metacommunity structure is highly context dependent from region to region. We rejected our primary hypotheses, pinning this lack of fit on the strong unpredictability of New Zealand’s dynamic stream ecosystems and fauna that has evolved to cope with these conditions. While local community structure turned over along this latitudinal gradient, metacommunity structure was highly context dependent and dispersal traits did not elucidate patterns. Moreover, the emergent metacommunity types exhibited no trends, nor did the important environmental variables. These results provide a cautionary tale for examining singular metacommunities. The considerable level of unexplained contingency suggests that any inferences drawn from one-off snapshot sampling may be misleading and further points to the need for more studies on temporal dynamics of metacommunity processes.
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spelling doaj.art-60007f3f1ed6486b8d9567628d3377172023-12-03T00:52:07ZengPeerJ Inc.PeerJ2167-83592018-05-016e489810.7717/peerj.4898Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?Jonathan D. Tonkin0Russell G. Death1Timo Muotka2Anna Astorga3David A. Lytle4Department of Integrative Biology, Oregon State University, Corvallis, OR, USAInstitute of Agriculture and Environment, Massey University, Palmerston North, New ZealandDepartment of Ecology, University of Oulu, Oulu, FinlandInstitute of Ecology and Biodiversity, P. Universidad Catolica de Chile & Centro de Investigación de Ecosistemas de la Patagonia, Coyhaique, ChileDepartment of Integrative Biology, Oregon State University, Corvallis, OR, USAThat biodiversity declines with latitude is well known, but whether a metacommunity process is behind this gradient has received limited attention. We tested the hypothesis that dispersal limitation is progressively replaced by mass effects with increasing latitude, along with a series of related hypotheses. We explored these hypotheses by examining metacommunity structure in stream invertebrate metacommunities spanning the length of New Zealand’s two largest islands (∼1,300 km), further disentangling the role of dispersal by deconstructing assemblages into strong and weak dispersers. Given the highly dynamic nature of New Zealand streams, our alternative hypothesis was that these systems are so unpredictable (at different stages of post-flood succession) that metacommunity structure is highly context dependent from region to region. We rejected our primary hypotheses, pinning this lack of fit on the strong unpredictability of New Zealand’s dynamic stream ecosystems and fauna that has evolved to cope with these conditions. While local community structure turned over along this latitudinal gradient, metacommunity structure was highly context dependent and dispersal traits did not elucidate patterns. Moreover, the emergent metacommunity types exhibited no trends, nor did the important environmental variables. These results provide a cautionary tale for examining singular metacommunities. The considerable level of unexplained contingency suggests that any inferences drawn from one-off snapshot sampling may be misleading and further points to the need for more studies on temporal dynamics of metacommunity processes.https://peerj.com/articles/4898.pdfMetacommunity structureMetacommunity typesEnvironmental stochasticityDispersalStream communityLatitudinal gradient
spellingShingle Jonathan D. Tonkin
Russell G. Death
Timo Muotka
Anna Astorga
David A. Lytle
Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
PeerJ
Metacommunity structure
Metacommunity types
Environmental stochasticity
Dispersal
Stream community
Latitudinal gradient
title Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
title_full Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
title_fullStr Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
title_full_unstemmed Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
title_short Do latitudinal gradients exist in New Zealand stream invertebrate metacommunities?
title_sort do latitudinal gradients exist in new zealand stream invertebrate metacommunities
topic Metacommunity structure
Metacommunity types
Environmental stochasticity
Dispersal
Stream community
Latitudinal gradient
url https://peerj.com/articles/4898.pdf
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