Snowmelt timing affects short‐term decomposition rates in an alpine snowbed

Abstract Alpine snowbed communities are characterized as having areas of longer lasting snow cover duration compared with the surrounding landscape. The predictable accumulation of deep and long‐lasting snow on lee side ridges drives a unique ecology, providing stable microclimatic conditions under...

Full description

Bibliographic Details
Main Authors: Susanna E. Venn, Haydn J. D. Thomas
Format: Article
Language:English
Published: Wiley 2021-03-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1002/ecs2.3393
_version_ 1818958719878168576
author Susanna E. Venn
Haydn J. D. Thomas
author_facet Susanna E. Venn
Haydn J. D. Thomas
author_sort Susanna E. Venn
collection DOAJ
description Abstract Alpine snowbed communities are characterized as having areas of longer lasting snow cover duration compared with the surrounding landscape. The predictable accumulation of deep and long‐lasting snow on lee side ridges drives a unique ecology, providing stable microclimatic conditions under the snow through winter, supplying meltwater in spring, and controlling many biological processes. The timing and rate of plant litter decomposition are key controls on the nutrient balance of snowbed communities, and are thought to be strongly driven by snow dynamics. However, little is known about how the patterns and timing of snowmelt affect decomposition, nor how long these effects last into the growing season. We investigated the influence of snowmelt timing on decomposition rates across an alpine snowbed community by burying standardized plant litter (rooibos and green tea), at three incubation times (whole year, winter+spring, and summer), across three snowmelt zones. Decomposition rate (as percent mass loss of tea) was significantly higher in early‐melting zones compared to late‐melting zones, particularly for the recalcitrant litter (rooibos tea). Decomposition was also affected by the season(s) of incubation and was greatest where tea was buried for the whole year, or only over summer, with winter   + spring only incubations decomposing the least. However, decomposition was more strongly influenced by litter quality (type of tea) than either the timing of snowmelt or seasonality. These results provide further understanding about how changes to the timing of snowmelt may in turn transform these rare and unique plant communities.
first_indexed 2024-12-20T11:30:13Z
format Article
id doaj.art-9a27d1d960d94982884a55c188c0c676
institution Directory Open Access Journal
issn 2150-8925
language English
last_indexed 2024-12-20T11:30:13Z
publishDate 2021-03-01
publisher Wiley
record_format Article
series Ecosphere
spelling doaj.art-9a27d1d960d94982884a55c188c0c6762022-12-21T19:42:15ZengWileyEcosphere2150-89252021-03-01123n/an/a10.1002/ecs2.3393Snowmelt timing affects short‐term decomposition rates in an alpine snowbedSusanna E. Venn0Haydn J. D. Thomas1Centre for Integrative Ecology School of Life and Environmental Sciences Deakin University Burwood Victoria3125AustraliaSchool of Geosciences University of Edinburgh EdinburghEH9 3FFUKAbstract Alpine snowbed communities are characterized as having areas of longer lasting snow cover duration compared with the surrounding landscape. The predictable accumulation of deep and long‐lasting snow on lee side ridges drives a unique ecology, providing stable microclimatic conditions under the snow through winter, supplying meltwater in spring, and controlling many biological processes. The timing and rate of plant litter decomposition are key controls on the nutrient balance of snowbed communities, and are thought to be strongly driven by snow dynamics. However, little is known about how the patterns and timing of snowmelt affect decomposition, nor how long these effects last into the growing season. We investigated the influence of snowmelt timing on decomposition rates across an alpine snowbed community by burying standardized plant litter (rooibos and green tea), at three incubation times (whole year, winter+spring, and summer), across three snowmelt zones. Decomposition rate (as percent mass loss of tea) was significantly higher in early‐melting zones compared to late‐melting zones, particularly for the recalcitrant litter (rooibos tea). Decomposition was also affected by the season(s) of incubation and was greatest where tea was buried for the whole year, or only over summer, with winter   + spring only incubations decomposing the least. However, decomposition was more strongly influenced by litter quality (type of tea) than either the timing of snowmelt or seasonality. These results provide further understanding about how changes to the timing of snowmelt may in turn transform these rare and unique plant communities.https://doi.org/10.1002/ecs2.3393climate changelitter decompositionsnowbed communitysnowmelt timingtea bag index
spellingShingle Susanna E. Venn
Haydn J. D. Thomas
Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
Ecosphere
climate change
litter decomposition
snowbed community
snowmelt timing
tea bag index
title Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
title_full Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
title_fullStr Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
title_full_unstemmed Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
title_short Snowmelt timing affects short‐term decomposition rates in an alpine snowbed
title_sort snowmelt timing affects short term decomposition rates in an alpine snowbed
topic climate change
litter decomposition
snowbed community
snowmelt timing
tea bag index
url https://doi.org/10.1002/ecs2.3393
work_keys_str_mv AT susannaevenn snowmelttimingaffectsshorttermdecompositionratesinanalpinesnowbed
AT haydnjdthomas snowmelttimingaffectsshorttermdecompositionratesinanalpinesnowbed