Biogeochemical Cycling and Sediment Ecology:
Oceanographic discontinuities (e. g. frontal systems, upwelling areas, ice edges) are often areas of enhanced biological productivity. Considerable research on the physics and biology of the physical boundaries defining these discontinues has been accomplished (see [I D. The interface between water...
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Weitere Verfasser: | , , |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Dordrecht
Springer Netherlands
1999
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Schriftenreihe: | NATO ASI Series, Series E: Applied Sciences
59 |
Schlagworte: | |
Online-Zugang: | BTU01 URL des Erstveröffentlichers |
Zusammenfassung: | Oceanographic discontinuities (e. g. frontal systems, upwelling areas, ice edges) are often areas of enhanced biological productivity. Considerable research on the physics and biology of the physical boundaries defining these discontinues has been accomplished (see [I D. The interface between water and sediment is the largest physical boundary in the ocean, but has not received a proportionate degree of attention. The purpose of the Nato Advanced Research Workshop (ARW) was to focus on soft-sediment systems by identifying deficiencies in our knowledge of these systems and defining key issues in the management of coastal sedimentary habitats. Marine sediments play important roles in the marine ecosystem and the biosphere. They provide food and habitat for many marine organisms, some of which are commercially important. More importantly from a global perspective, marine sediments also provide "ecosystem goods and services" [2J. Organic matter from primary production in the water column and contaminants scavenged by particles accumulate in sediments where their fate is determined by sediment processes such as bioturbation and biogeochemical cycling. Nutrients are regenerated and contaminants degraded in sediments. Under some conditions, carbon accumulates in coastal and shelf sediments and may by removed from the carbon cycle for millions of years, having a potentially significant impact on global climate change. Sediments also protect coasts. The economic value of services provided by coastal areas has recently been estimated to be on the order of $12,568 9 10 y" [3J, far in excess of the global GNP. |
Beschreibung: | 1 Online-Ressource (XII, 236 p) |
ISBN: | 9789401146494 |
DOI: | 10.1007/978-94-011-4649-4 |
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520 | |a Oceanographic discontinuities (e. g. frontal systems, upwelling areas, ice edges) are often areas of enhanced biological productivity. Considerable research on the physics and biology of the physical boundaries defining these discontinues has been accomplished (see [I D. The interface between water and sediment is the largest physical boundary in the ocean, but has not received a proportionate degree of attention. The purpose of the Nato Advanced Research Workshop (ARW) was to focus on soft-sediment systems by identifying deficiencies in our knowledge of these systems and defining key issues in the management of coastal sedimentary habitats. Marine sediments play important roles in the marine ecosystem and the biosphere. They provide food and habitat for many marine organisms, some of which are commercially important. More importantly from a global perspective, marine sediments also provide "ecosystem goods and services" [2J. Organic matter from primary production in the water column and contaminants scavenged by particles accumulate in sediments where their fate is determined by sediment processes such as bioturbation and biogeochemical cycling. Nutrients are regenerated and contaminants degraded in sediments. Under some conditions, carbon accumulates in coastal and shelf sediments and may by removed from the carbon cycle for millions of years, having a potentially significant impact on global climate change. Sediments also protect coasts. The economic value of services provided by coastal areas has recently been estimated to be on the order of $12,568 9 10 y" [3J, far in excess of the global GNP. | ||
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Datensatz im Suchindex
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any_adam_object | |
author2 | Gray, John S. Ambrose, William Szaniawska, Anna |
author2_role | edt edt edt |
author2_variant | j s g js jsg w a wa a s as |
author_facet | Gray, John S. Ambrose, William Szaniawska, Anna |
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dewey-full | 570 |
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dewey-ones | 570 - Biology |
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discipline | Biologie |
doi_str_mv | 10.1007/978-94-011-4649-4 |
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genre | 1\p (DE-588)1071861417 Konferenzschrift 1997 Hela gnd-content |
genre_facet | Konferenzschrift 1997 Hela |
id | DE-604.BV045176638 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T08:10:45Z |
institution | BVB |
isbn | 9789401146494 |
language | English |
oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030565868 |
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physical | 1 Online-Ressource (XII, 236 p) |
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publisher | Springer Netherlands |
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series2 | NATO ASI Series, Series E: Applied Sciences |
spelling | Biogeochemical Cycling and Sediment Ecology edited by John S. Gray, William Ambrose, Anna Szaniawska Proceedings of the NATO Advanced Research Workshop on Biochemical Cycling in Marine Sediments, held in Hel, Poland, August 1997 Dordrecht Springer Netherlands 1999 1 Online-Ressource (XII, 236 p) txt rdacontent c rdamedia cr rdacarrier NATO ASI Series, Series E: Applied Sciences 59 Oceanographic discontinuities (e. g. frontal systems, upwelling areas, ice edges) are often areas of enhanced biological productivity. Considerable research on the physics and biology of the physical boundaries defining these discontinues has been accomplished (see [I D. The interface between water and sediment is the largest physical boundary in the ocean, but has not received a proportionate degree of attention. The purpose of the Nato Advanced Research Workshop (ARW) was to focus on soft-sediment systems by identifying deficiencies in our knowledge of these systems and defining key issues in the management of coastal sedimentary habitats. Marine sediments play important roles in the marine ecosystem and the biosphere. They provide food and habitat for many marine organisms, some of which are commercially important. More importantly from a global perspective, marine sediments also provide "ecosystem goods and services" [2J. Organic matter from primary production in the water column and contaminants scavenged by particles accumulate in sediments where their fate is determined by sediment processes such as bioturbation and biogeochemical cycling. Nutrients are regenerated and contaminants degraded in sediments. Under some conditions, carbon accumulates in coastal and shelf sediments and may by removed from the carbon cycle for millions of years, having a potentially significant impact on global climate change. Sediments also protect coasts. The economic value of services provided by coastal areas has recently been estimated to be on the order of $12,568 9 10 y" [3J, far in excess of the global GNP. Life Sciences Life Sciences, general Environmental Science and Engineering Freshwater & Marine Ecology Oceanography Geochemistry Ecology Life sciences Environmental sciences Aquatic ecology Kreislauf (DE-588)4165608-8 gnd rswk-swf Meeressediment (DE-588)4134766-3 gnd rswk-swf Biogeochemie (DE-588)4125243-3 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 1997 Hela gnd-content Meeressediment (DE-588)4134766-3 s Biogeochemie (DE-588)4125243-3 s Kreislauf (DE-588)4165608-8 s 2\p DE-604 Gray, John S. edt Ambrose, William edt Szaniawska, Anna edt Erscheint auch als Druck-Ausgabe 9789401059626 https://doi.org/10.1007/978-94-011-4649-4 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
spellingShingle | Biogeochemical Cycling and Sediment Ecology Life Sciences Life Sciences, general Environmental Science and Engineering Freshwater & Marine Ecology Oceanography Geochemistry Ecology Life sciences Environmental sciences Aquatic ecology Kreislauf (DE-588)4165608-8 gnd Meeressediment (DE-588)4134766-3 gnd Biogeochemie (DE-588)4125243-3 gnd |
subject_GND | (DE-588)4165608-8 (DE-588)4134766-3 (DE-588)4125243-3 (DE-588)1071861417 |
title | Biogeochemical Cycling and Sediment Ecology |
title_alt | Proceedings of the NATO Advanced Research Workshop on Biochemical Cycling in Marine Sediments, held in Hel, Poland, August 1997 |
title_auth | Biogeochemical Cycling and Sediment Ecology |
title_exact_search | Biogeochemical Cycling and Sediment Ecology |
title_full | Biogeochemical Cycling and Sediment Ecology edited by John S. Gray, William Ambrose, Anna Szaniawska |
title_fullStr | Biogeochemical Cycling and Sediment Ecology edited by John S. Gray, William Ambrose, Anna Szaniawska |
title_full_unstemmed | Biogeochemical Cycling and Sediment Ecology edited by John S. Gray, William Ambrose, Anna Szaniawska |
title_short | Biogeochemical Cycling and Sediment Ecology |
title_sort | biogeochemical cycling and sediment ecology |
topic | Life Sciences Life Sciences, general Environmental Science and Engineering Freshwater & Marine Ecology Oceanography Geochemistry Ecology Life sciences Environmental sciences Aquatic ecology Kreislauf (DE-588)4165608-8 gnd Meeressediment (DE-588)4134766-3 gnd Biogeochemie (DE-588)4125243-3 gnd |
topic_facet | Life Sciences Life Sciences, general Environmental Science and Engineering Freshwater & Marine Ecology Oceanography Geochemistry Ecology Life sciences Environmental sciences Aquatic ecology Kreislauf Meeressediment Biogeochemie Konferenzschrift 1997 Hela |
url | https://doi.org/10.1007/978-94-011-4649-4 |
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