Downward particle fluxes and sediment accumulation rates in the Western Bransfield Strait: implications for carbon cycle studies in Antarctic marginal seas

A. Palanques; E. Isla; P. Masqué; P. Puig; J.A. Sanchez-Cabeza; J.M Gili; J. Guillén

doi:10.1357/00222400260497525

Downward particle fluxes and sediment accumulation rates in the Western Bransfield Strait: implications for carbon cycle studies in Antarctic marginal seas

A. Palanques, E. Isla, P. Masqué, P. Puig, J.A. Sanchez-Cabeza, J.M Gili, J. Guillén

Departament de Física

Producció científica: Contribució a revista › Article › Recerca

21 Cites (Scopus)

Idioma original	Anglès
Pàgines (de-a)	347-365
Revista	Journal of Marine Research
Volum	60
Número	2
DOIs	https://doi.org/10.1357/00222400260497525
Estat de la publicació	Publicada - 1 de gen. 2002

Accés al document

10.1357/00222400260497525

Altres arxius i enllaços

https://www.scopus.com/pages/publications/0036077782

Com citar-ho

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title = "Downward particle fluxes and sediment accumulation rates in the Western Bransfield Strait: implications for carbon cycle studies in Antarctic marginal seas",

author = "A. Palanques and E. Isla and P. Masqu{\'e} and P. Puig and J.A. Sanchez-Cabeza and J.M Gili and J. Guill{\'e}n",

year = "2002",

month = jan,

day = "1",

doi = "10.1357/00222400260497525",

language = "English",

volume = "60",

pages = "347--365",

journal = "Journal of Marine Research",

issn = "0022-2402",

publisher = "Yale University",

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T1 - Downward particle fluxes and sediment accumulation rates in the Western Bransfield Strait: implications for carbon cycle studies in Antarctic marginal seas

AU - Palanques, A.

AU - Isla, E.

AU - Masqué, P.

AU - Puig, P.

AU - Sanchez-Cabeza, J.A.

AU - Gili, J.M

AU - Guillén, J.

PY - 2002/1/1

Y1 - 2002/1/1

UR - https://www.scopus.com/pages/publications/0036077782

U2 - 10.1357/00222400260497525

DO - 10.1357/00222400260497525

M3 - Article

SN - 0022-2402

VL - 60

SP - 347

EP - 365

JO - Journal of Marine Research

JF - Journal of Marine Research

IS - 2

ER -