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|a (DE-627)JST114443238
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|a (JST)24876149
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|a DE-627
|b ger
|c DE-627
|e rakwb
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|a eng
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|a Krumhansl, Kira A.
|e verfasserin
|4 aut
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|a Production and fate of kelp detritus
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|c 2012
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|a Text
|b txt
|2 rdacontent
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|a Computermedien
|b c
|2 rdamedia
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|a Online-Ressource
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|a ABSTRACT: The flow of detritus between habitats is an important form of connectivity that affects regional productivity and the spatial organization of marine ecosystems. Kelps form highly productive beds or forests that produce detritus through incremental blade erosion, fragmentation of blades, and dislodgement of whole fronds and thalli. Rates of detrital production range from 8 to 2657 g C m−2yr−1for blade erosion and fragmentation, and from 22 to 839 g C m−2yr−1for loss of fronds and thalli. The estimated global average rate of detrital production by kelps is 706 g C m−2yr−1, accounting for 82% of annual kelp productivity. Detrital production rates are regulated by current and wave-driven hydrodynamic forces and are highest during severe storms and following blade weakening through damage by grazers and encrusting epibionts. Detritus settles within kelp beds or forests and is exported to neighboring or distant habitats, including sandy beaches, rocky intertidal shores, rocky and sedimentary subtidal areas, and the deep sea. Exported kelp detritus can provide a significant resource subsidy and enhance secondary production in these communities ranging from tens of meters to hundreds of kilometers from the source of production. Loss of kelp biomass is occurring worldwide through the combined effects of climate change, pollution, fishing, and harvesting of kelp, which can depress rates of detrital production and subsidy to adjacent communities, with large-scale consequences for productivity.
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|a © Inter-Research 2012
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|a Kelp bed
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|a Kelp forest
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|a Connectivity
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|a Detritus
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|a Resource subsidy
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|a Local-regional productivity
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|a Biological sciences
|x Ecology
|x Population ecology
|x Synecology
|x Biocenosis
|x Aquatic communities
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|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Landforms
|x Coastal landforms
|x Beaches
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|a Biological sciences
|x Biology
|x Zoology
|x Animals
|x Invertebrates
|x Aquatic invertebrates
|x Echinoderms
|x Sea urchins
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|a Biological sciences
|x Ecology
|x Ecosystems
|x Aquatic ecosystems
|x Marine ecosystems
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|a Economics
|x Economic policy
|x Public finance
|x Subsidies
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|a Biological sciences
|x Ecology
|x Aquatic ecology
|x Marine ecology
|x Coastal ecology
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|a Business
|x Business economics
|x Commercial production
|x Productivity
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|a Biological sciences
|x Biology
|x Botany
|x Plant ecology
|x Forest ecology
|x Forest ecosystems
|x Forest habitats
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|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Bodies of water
|x Seas
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|a Biological sciences
|x Biology
|x Botany
|x Marine botany
|x Aquatic plants
|x Macrophytes
|x REVIEW
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|a research-article
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|a Scheibling, Robert E.
|e verfasserin
|4 aut
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|i Enthalten in
|t Marine Ecology Progress Series
|d Inter-Research, 1979
|g 467(2012) vom: Okt., Seite 281-302
|w (DE-627)320617998
|w (DE-600)2022265-8
|x 16161599
|7 nnns
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|g volume:467
|g year:2012
|g month:10
|g pages:281-302
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|u https://www.jstor.org/stable/24876149
|3 Volltext
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|d 467
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|h 281-302
|