Response of Bosmina to climate variability and reduced nutrient loading in a large lake

The long-term dynamics of the cladoceran Bosmina spp. were analysed in Lake Constance during the study period 1979 1998. During this period the lake ecosystem has been influenced strongly by changes in nutrient inflow (oligotrophication) and by climate variability associated with the North Atlantic...

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Published in:Limnologica
Main Authors: Straile, Dietmar, Müller, Helga
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
Online Access:http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-109023
https://doi.org/10.1016/j.limno.2009.11.004
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spelling ftubkonstanz:oai:kops.uni-konstanz.de:123456789/7097 2024-02-11T10:06:16+01:00 Response of Bosmina to climate variability and reduced nutrient loading in a large lake Straile, Dietmar Müller, Helga 2010 application/pdf http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-109023 https://doi.org/10.1016/j.limno.2009.11.004 eng eng http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-109023 http://dx.doi.org/10.1016/j.limno.2009.11.004 321015401 https://rightsstatements.org/page/InC/1.0/ Limnologica. 2010, 40(2), pp. 92-96. ISSN 0075-9511. Available under: doi:10.1016/j.limno.2009.11.004 North Atlantic Oscillation Oligotrophication Spring bloom Seasonal dynamics Long-term time series ddc:570 doc-type:article doc-type:Text 2010 ftubkonstanz https://doi.org/10.1016/j.limno.2009.11.004 2024-01-21T23:51:35Z The long-term dynamics of the cladoceran Bosmina spp. were analysed in Lake Constance during the study period 1979 1998. During this period the lake ecosystem has been influenced strongly by changes in nutrient inflow (oligotrophication) and by climate variability associated with the North Atlantic Oscillation. Bosmina abundances declined strongly during the study period presumably as an indirect consequence of the reduced P loading of the lake. A detailed seasonally resolved analysis of Bosmina dynamics revealed that its abundance decline occurred throughout the year with the exception of the spring period. The lack of a population decline during spring may be attributed to the seasonal absence of the factor, e.g., food limitation and/or predation control by invertebrates causing the population decline. Additionally, climate variability had its strongest influence on Bosmina dynamics during spring and large climate-associated variability of Bosmina may have decreased the power to detect a significant reduction in spring Bosmina abundances with oligotrophication. However, when we account for the confounding influence of climate variability, the effects of oligotrophication are revealed more clearly also during the spring period. Likewise, the detectability of the influence of climate variability on spring Bosmina dynamics increases when accounting for the reduction of abundances in the course of oligotrophication. published published Article in Journal/Newspaper North Atlantic North Atlantic oscillation KOPS - The Institutional Repository of the University of Konstanz Limnologica 40 2 92 96
institution Open Polar
collection KOPS - The Institutional Repository of the University of Konstanz
op_collection_id ftubkonstanz
language English
topic North Atlantic Oscillation Oligotrophication
Spring bloom
Seasonal dynamics
Long-term time series
ddc:570
spellingShingle North Atlantic Oscillation Oligotrophication
Spring bloom
Seasonal dynamics
Long-term time series
ddc:570
Straile, Dietmar
Müller, Helga
Response of Bosmina to climate variability and reduced nutrient loading in a large lake
topic_facet North Atlantic Oscillation Oligotrophication
Spring bloom
Seasonal dynamics
Long-term time series
ddc:570
description The long-term dynamics of the cladoceran Bosmina spp. were analysed in Lake Constance during the study period 1979 1998. During this period the lake ecosystem has been influenced strongly by changes in nutrient inflow (oligotrophication) and by climate variability associated with the North Atlantic Oscillation. Bosmina abundances declined strongly during the study period presumably as an indirect consequence of the reduced P loading of the lake. A detailed seasonally resolved analysis of Bosmina dynamics revealed that its abundance decline occurred throughout the year with the exception of the spring period. The lack of a population decline during spring may be attributed to the seasonal absence of the factor, e.g., food limitation and/or predation control by invertebrates causing the population decline. Additionally, climate variability had its strongest influence on Bosmina dynamics during spring and large climate-associated variability of Bosmina may have decreased the power to detect a significant reduction in spring Bosmina abundances with oligotrophication. However, when we account for the confounding influence of climate variability, the effects of oligotrophication are revealed more clearly also during the spring period. Likewise, the detectability of the influence of climate variability on spring Bosmina dynamics increases when accounting for the reduction of abundances in the course of oligotrophication. published published
format Article in Journal/Newspaper
author Straile, Dietmar
Müller, Helga
author_facet Straile, Dietmar
Müller, Helga
author_sort Straile, Dietmar
title Response of Bosmina to climate variability and reduced nutrient loading in a large lake
title_short Response of Bosmina to climate variability and reduced nutrient loading in a large lake
title_full Response of Bosmina to climate variability and reduced nutrient loading in a large lake
title_fullStr Response of Bosmina to climate variability and reduced nutrient loading in a large lake
title_full_unstemmed Response of Bosmina to climate variability and reduced nutrient loading in a large lake
title_sort response of bosmina to climate variability and reduced nutrient loading in a large lake
publishDate 2010
url http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-109023
https://doi.org/10.1016/j.limno.2009.11.004
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Limnologica. 2010, 40(2), pp. 92-96. ISSN 0075-9511. Available under: doi:10.1016/j.limno.2009.11.004
op_relation http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-109023
http://dx.doi.org/10.1016/j.limno.2009.11.004
321015401
op_rights https://rightsstatements.org/page/InC/1.0/
op_doi https://doi.org/10.1016/j.limno.2009.11.004
container_title Limnologica
container_volume 40
container_issue 2
container_start_page 92
op_container_end_page 96
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