macdonald robie (21 risultati)

Pamphlet. Condizione: Very Good. Vol 48, No 2, pp. 118-129, Map, Illus, 4to, Extracted from orig vol, thus begins with title page, trimmed & stapled pamphlet, else VG.

Condizione: New. pp. xix + 383.

Taschenbuch. Condizione: Neu. The Organic Carbon Cycle in the Arctic Ocean | Rüdiger Stein (u. a.) | Taschenbuch | xix | Englisch | 2013 | Springer | EAN 9783642623516 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.

Condizione: New. pp. xix + 383, Map (Some Col.).

Taschenbuch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute 1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; 1 Hedges et al. 1997). On average,only about 0. 1 0. 2 Gt y of the organic carbon supplied to the world s oceans has been buried in Holocene sediments, with perhaps 85 90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments.

Buch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute 1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; 1 Hedges et al. 1997). On average,only about 0. 1 0. 2 Gt y of the organic carbon supplied to the world s oceans has been buried in Holocene sediments, with perhaps 85 90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments.

Hardcover. Condizione: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Paperback. Condizione: Brand New. 363 pages. 10.50x7.50x1.00 inches. In Stock.

Paperback. Condizione: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Condizione: new. Questo è un articolo print on demand.

Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute 1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; 1 Hedges et al. 1997). On average,only about 0. 1 0. 2 Gt y of the organic carbon supplied to the world s oceans has been buried in Holocene sediments, with perhaps 85 90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments. 384 pp. Englisch.

Buch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute 1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; 1 Hedges et al. 1997). On average,only about 0. 1 0. 2 Gt y of the organic carbon supplied to the world s oceans has been buried in Holocene sediments, with perhaps 85 90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments. 384 pp. Englisch.

Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Comprehensive overview&nbspof organic-carbon sources written by both editors, who&nbsphave extensive experience in oceanographic research in the Atlantic1 The Arctic Ocean: Boundary Conditions and Background Information.- 1.1 Physiography and Bath.

Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Comprehensive overview&nbspof organic-carbon sources written by both editors, who&nbsphave extensive experience in oceanographic research in the Atlantic1 The Arctic Ocean: Boundary Conditions and Background Information.- 1.1 Physiography and Bath.

Buch. Condizione: Neu. The Organic Carbon Cycle in the Arctic Ocean | Robie W. Macdonald (u. a.) | Buch | xix | Englisch | 2003 | Springer | EAN 9783540011538 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu Print on Demand.

Buch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world¿s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute ¿1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; ¿1 Hedges et al. 1997). On average,only about 0. 1¿0. 2 Gt y of the organic carbon supplied to the world¿s oceans has been buried in Holocene sediments, with perhaps 85¿90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments.Springer-Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 384 pp. Englisch.

Taschenbuch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The flux,preservation,and accumulation of organic carbon in marine systems are controlled by various mechanisms including primary p- duction of the surface water,supply of terrigenous organic matter from the surrounding continents, biogeochemical processes in the water column and at the seafloor, and sedimentation rate. For the world¿s oceans,phytoplankton productivity is by far the largest organic carbon 9 source,estimated to be about 30 to 50 Gt (10 tonnes) per year (Berger et al. 1989; Hedges and Keil 1995). By comparison, rivers contribute ¿1 about 0. 15 to 0. 23 Gt y of particulate organic carbon (Ittekkot 1988; ¿1 Hedges et al. 1997). On average,only about 0. 1¿0. 2 Gt y of the organic carbon supplied to the world¿s oceans has been buried in Holocene sediments, with perhaps 85¿90% of that being deposited in deltaic, shelf and upper slope sediments (Romankevich 1984; Berner 1989; Hedges and Keil 1995). To refine the global ocean carbon budget in general and,specifically,to quantify organic carbon burial because it is so important for climatic change, we need detailed measurements of the organic carbon flux in all ocean environments, especially for c- tinental margins (e. g. ,Liu et al. ,2000). With the notable exception of the Arctic Ocean, data have been available for some time on organic carbon sources, pathways and burial in a variety of ocean envir- ments.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 384 pp. Englisch.

Condizione: New. Print on Demand pp. xix + 383.

Condizione: New. Print on Demand pp. xix + 383 Illus., Map (Some Col.).

Condizione: New. PRINT ON DEMAND pp. xix + 383.

Condizione: New. PRINT ON DEMAND pp. xix + 383.