Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet
Abstract A widely examined predictive model of invertebrate community dynamics in glacial‐melt streams describes longitudinal changes in community structure with changing water temperature and channel stability with increasing distance from glaciers. Previous studies conducted in Europe, Greenland,...
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crwiley:10.1111/fwb.13716 2024-06-02T08:07:03+00:00 Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet Fair, Heather Smiley, Peter C. Lanno, Roman National Science Foundation 2021 http://dx.doi.org/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/pdf/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/am-pdf/10.1111/fwb.13716 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#am http://onlinelibrary.wiley.com/termsAndConditions#vor Freshwater Biology volume 66, issue 7, page 1282-1295 ISSN 0046-5070 1365-2427 journal-article 2021 crwiley https://doi.org/10.1111/fwb.13716 2024-05-03T11:08:41Z Abstract A widely examined predictive model of invertebrate community dynamics in glacial‐melt streams describes longitudinal changes in community structure with changing water temperature and channel stability with increasing distance from glaciers. Previous studies conducted in Europe, Greenland, New Zealand, and South America have supported the predictions of the invertebrate model and contributed to its refinement. However, none has evaluated if the model fits invertebrate community dynamics over a full range of distances from the glacier and water temperature conditions within glacial‐melt streams in southeast Tibet. We sampled invertebrates and measured water temperature, specific conductivity, turbidity, and associated glacier‐related variables within 14 sites in three subalpine glacial‐melt catchments in southeastern Tibet's Three Parallel Rivers region during 2010, 2011, 2013, and 2015. Our sites encompassed a temperature gradient from the upstream metakryal sites (maximum summer water temperature <2°C) to the furthest downstream site (maximum summer temperature >10°C) near the Mekong River. We evaluated the relationships of invertebrate community structure with in situ water temperature and channel stability which are the focal habitat variables in the invertebrate model. The additional habitat variables of distance from the glacier, glacier size, conductivity, and turbidity were evaluated to see if these were more important determinants of community structure than in situ water temperature and channel stability. Minimum and in situ water temperatures were positively correlated with distance from the glacier but Pfankuch Channel Stability Index bottom scores were not. Thus, the physical template within our study area differed from the expected template of the invertebrate model. Similar to the invertebrate model, in situ water temperature by itself or combined with Pfankuch index best explained five invertebrate response variables. In contrast with the invertebrate model, conductivity and ... Article in Journal/Newspaper glacier Greenland Wiley Online Library Greenland New Zealand Freshwater Biology 66 7 1282 1295 |
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Wiley Online Library |
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English |
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Abstract A widely examined predictive model of invertebrate community dynamics in glacial‐melt streams describes longitudinal changes in community structure with changing water temperature and channel stability with increasing distance from glaciers. Previous studies conducted in Europe, Greenland, New Zealand, and South America have supported the predictions of the invertebrate model and contributed to its refinement. However, none has evaluated if the model fits invertebrate community dynamics over a full range of distances from the glacier and water temperature conditions within glacial‐melt streams in southeast Tibet. We sampled invertebrates and measured water temperature, specific conductivity, turbidity, and associated glacier‐related variables within 14 sites in three subalpine glacial‐melt catchments in southeastern Tibet's Three Parallel Rivers region during 2010, 2011, 2013, and 2015. Our sites encompassed a temperature gradient from the upstream metakryal sites (maximum summer water temperature <2°C) to the furthest downstream site (maximum summer temperature >10°C) near the Mekong River. We evaluated the relationships of invertebrate community structure with in situ water temperature and channel stability which are the focal habitat variables in the invertebrate model. The additional habitat variables of distance from the glacier, glacier size, conductivity, and turbidity were evaluated to see if these were more important determinants of community structure than in situ water temperature and channel stability. Minimum and in situ water temperatures were positively correlated with distance from the glacier but Pfankuch Channel Stability Index bottom scores were not. Thus, the physical template within our study area differed from the expected template of the invertebrate model. Similar to the invertebrate model, in situ water temperature by itself or combined with Pfankuch index best explained five invertebrate response variables. In contrast with the invertebrate model, conductivity and ... |
author2 |
National Science Foundation |
format |
Article in Journal/Newspaper |
author |
Fair, Heather Smiley, Peter C. Lanno, Roman |
spellingShingle |
Fair, Heather Smiley, Peter C. Lanno, Roman Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
author_facet |
Fair, Heather Smiley, Peter C. Lanno, Roman |
author_sort |
Fair, Heather |
title |
Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
title_short |
Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
title_full |
Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
title_fullStr |
Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
title_full_unstemmed |
Determinants of invertebrate community structure in glacial‐melt streams of southeast Tibet |
title_sort |
determinants of invertebrate community structure in glacial‐melt streams of southeast tibet |
publisher |
Wiley |
publishDate |
2021 |
url |
http://dx.doi.org/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/pdf/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/fwb.13716 https://onlinelibrary.wiley.com/doi/am-pdf/10.1111/fwb.13716 |
geographic |
Greenland New Zealand |
geographic_facet |
Greenland New Zealand |
genre |
glacier Greenland |
genre_facet |
glacier Greenland |
op_source |
Freshwater Biology volume 66, issue 7, page 1282-1295 ISSN 0046-5070 1365-2427 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#am http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/fwb.13716 |
container_title |
Freshwater Biology |
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66 |
container_issue |
7 |
container_start_page |
1282 |
op_container_end_page |
1295 |
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1800752064826966016 |