Effects of Ocean Acidification on Sediment Fauna

The vast majority of the seafloor is covered not in rocky or biogenic reefs but in unconsolidated sediments and, consequently, the majority of marine biodiversity consists of invertebrates either residing in (infauna) or on (epifauna) sediments (Snelgrove 1999). The biodiversity within these sedimen...

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Main Authors: Widdicombe, Stephen, Spicer, John I.
Format: Book Part
Language:unknown
Published: Oxford University Press 2011
Subjects:
Online Access:http://dx.doi.org/10.1093/oso/9780199591091.003.0014
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spelling croxfordunivpr:10.1093/oso/9780199591091.003.0014 2023-11-05T03:44:27+01:00 Effects of Ocean Acidification on Sediment Fauna Widdicombe, Stephen Spicer, John I. 2011 http://dx.doi.org/10.1093/oso/9780199591091.003.0014 unknown Oxford University Press Ocean Acidification book-chapter 2011 croxfordunivpr https://doi.org/10.1093/oso/9780199591091.003.0014 2023-10-06T10:41:33Z The vast majority of the seafloor is covered not in rocky or biogenic reefs but in unconsolidated sediments and, consequently, the majority of marine biodiversity consists of invertebrates either residing in (infauna) or on (epifauna) sediments (Snelgrove 1999). The biodiversity within these sediments is a result of complex interactions between the underlying environmental conditions (e.g. depth, temperature, organic supply, and granulometry) and the biological interactions operating between organisms (e.g. predation and competition). Not only are sediments important depositories of biodiversity but they are also critical components in many key ecosystem functions. Nowhere is this more apparent than in shallow coastal seas and oceans which, despite covering less than 10% of the earth’s surface, deliver up to 30% of marine production and 90% of marine fisheries (Gattuso et al. 1998). These areas are also the site for 80% of organic matter burial and 90% of sedimentary mineralization and nutrient–sediment biogeochemical processes. They also act as the sink for up to 90% of the suspended load in the world’s rivers and the many associated contaminants this material contains (Gattuso et al. 1998). Human beings depend heavily on the goods and services provided, for free, by the marine realm (Hassan et al. 2005 ) and it is no coincidence that nearly 70% of all humans live within 60 km of the sea or that 75% of all cities with more than 10 million inhabitants are in the coastal zone (Small and Nicholls 2003; McGranahan et al. 2007) Given these facts, it is clear that any broad-scale environmental impact that affects the diversity, structure, and function of sediment ecosystems could have a considerable impact on human health and well-being. It is therefore essential that the impacts of ocean acidification on sediment fauna, and the ecosystem functions they support, are adequately considered. This chapter will first describe the geochemical environment within which sediment organisms live. It will then explore the role ... Book Part Ocean acidification Oxford University Press (via Crossref)
institution Open Polar
collection Oxford University Press (via Crossref)
op_collection_id croxfordunivpr
language unknown
description The vast majority of the seafloor is covered not in rocky or biogenic reefs but in unconsolidated sediments and, consequently, the majority of marine biodiversity consists of invertebrates either residing in (infauna) or on (epifauna) sediments (Snelgrove 1999). The biodiversity within these sediments is a result of complex interactions between the underlying environmental conditions (e.g. depth, temperature, organic supply, and granulometry) and the biological interactions operating between organisms (e.g. predation and competition). Not only are sediments important depositories of biodiversity but they are also critical components in many key ecosystem functions. Nowhere is this more apparent than in shallow coastal seas and oceans which, despite covering less than 10% of the earth’s surface, deliver up to 30% of marine production and 90% of marine fisheries (Gattuso et al. 1998). These areas are also the site for 80% of organic matter burial and 90% of sedimentary mineralization and nutrient–sediment biogeochemical processes. They also act as the sink for up to 90% of the suspended load in the world’s rivers and the many associated contaminants this material contains (Gattuso et al. 1998). Human beings depend heavily on the goods and services provided, for free, by the marine realm (Hassan et al. 2005 ) and it is no coincidence that nearly 70% of all humans live within 60 km of the sea or that 75% of all cities with more than 10 million inhabitants are in the coastal zone (Small and Nicholls 2003; McGranahan et al. 2007) Given these facts, it is clear that any broad-scale environmental impact that affects the diversity, structure, and function of sediment ecosystems could have a considerable impact on human health and well-being. It is therefore essential that the impacts of ocean acidification on sediment fauna, and the ecosystem functions they support, are adequately considered. This chapter will first describe the geochemical environment within which sediment organisms live. It will then explore the role ...
format Book Part
author Widdicombe, Stephen
Spicer, John I.
spellingShingle Widdicombe, Stephen
Spicer, John I.
Effects of Ocean Acidification on Sediment Fauna
author_facet Widdicombe, Stephen
Spicer, John I.
author_sort Widdicombe, Stephen
title Effects of Ocean Acidification on Sediment Fauna
title_short Effects of Ocean Acidification on Sediment Fauna
title_full Effects of Ocean Acidification on Sediment Fauna
title_fullStr Effects of Ocean Acidification on Sediment Fauna
title_full_unstemmed Effects of Ocean Acidification on Sediment Fauna
title_sort effects of ocean acidification on sediment fauna
publisher Oxford University Press
publishDate 2011
url http://dx.doi.org/10.1093/oso/9780199591091.003.0014
genre Ocean acidification
genre_facet Ocean acidification
op_source Ocean Acidification
op_doi https://doi.org/10.1093/oso/9780199591091.003.0014
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