Publication

Efficiency of carbon removal per added iron in ocean iron fertilization

de Baar, H. J. W., Gerringa, L. J. A., Laan, P. & Timmermans, K. R., 29-Jul-2008, In : Marine Ecology Progress Series. 364, p. 269-282 14 p.

Research output: Contribution to journalArticleAcademicpeer-review

APA

de Baar, H. J. W., Gerringa, L. J. A., Laan, P., & Timmermans, K. R. (2008). Efficiency of carbon removal per added iron in ocean iron fertilization. Marine Ecology Progress Series, 364, 269-282. https://doi.org/10.3354/meps07548

Author

de Baar, Hein J. W. ; Gerringa, Loes J. A. ; Laan, Patrick ; Timmermans, Klaas R. / Efficiency of carbon removal per added iron in ocean iron fertilization. In: Marine Ecology Progress Series. 2008 ; Vol. 364. pp. 269-282.

Harvard

de Baar, HJW, Gerringa, LJA, Laan, P & Timmermans, KR 2008, 'Efficiency of carbon removal per added iron in ocean iron fertilization', Marine Ecology Progress Series, vol. 364, pp. 269-282. https://doi.org/10.3354/meps07548

Standard

Efficiency of carbon removal per added iron in ocean iron fertilization. / de Baar, Hein J. W.; Gerringa, Loes J. A.; Laan, Patrick; Timmermans, Klaas R.

In: Marine Ecology Progress Series, Vol. 364, 29.07.2008, p. 269-282.

Research output: Contribution to journalArticleAcademicpeer-review

Vancouver

de Baar HJW, Gerringa LJA, Laan P, Timmermans KR. Efficiency of carbon removal per added iron in ocean iron fertilization. Marine Ecology Progress Series. 2008 Jul 29;364:269-282. https://doi.org/10.3354/meps07548


BibTeX

@article{3afd7612cb6742908d6f21e9d8a4c109,
title = "Efficiency of carbon removal per added iron in ocean iron fertilization",
abstract = "The major response to ocean iron fertilization is by large diatoms, which at Fe-replete ambient seawater show an optimum C:Fe elemental ratio of similar to 23 000 and a higher ratio of similar to 160 000 or more under Fe-limited conditions. The efficiency of CO2 drawdown during the several weeks of artificial fertilization experiments with concomitant observations is in the range of 100 <(CO2:Fe) <1000 and is unknown in direction (positive or negative) and magnitude in the period after observations. The efficiency of biogenic carbon export into deeper water layers ranges from similar to 650 <(C:Fe)(export) ",
keywords = "iron, fertilization, ocean, efficiency, carbon, export, diatoms, SOUTHERN-OCEAN, PHYTOPLANKTON BLOOM, MARINE-PHYTOPLANKTON, ROSS SEA, ENRICHMENT EXPERIMENT, NORTHEAST PACIFIC, LIGHT LIMITATION, EXPERIMENT SOFEX, ATLANTIC-OCEAN, DISSOLVED IRON",
author = "{de Baar}, {Hein J. W.} and Gerringa, {Loes J. A.} and Patrick Laan and Timmermans, {Klaas R.}",
year = "2008",
month = jul,
day = "29",
doi = "10.3354/meps07548",
language = "English",
volume = "364",
pages = "269--282",
journal = "Marine Ecology Progress Series",
issn = "0171-8630",
publisher = "INTER-RESEARCH",

}

RIS

TY - JOUR

T1 - Efficiency of carbon removal per added iron in ocean iron fertilization

AU - de Baar, Hein J. W.

AU - Gerringa, Loes J. A.

AU - Laan, Patrick

AU - Timmermans, Klaas R.

PY - 2008/7/29

Y1 - 2008/7/29

N2 - The major response to ocean iron fertilization is by large diatoms, which at Fe-replete ambient seawater show an optimum C:Fe elemental ratio of similar to 23 000 and a higher ratio of similar to 160 000 or more under Fe-limited conditions. The efficiency of CO2 drawdown during the several weeks of artificial fertilization experiments with concomitant observations is in the range of 100 <(CO2:Fe) <1000 and is unknown in direction (positive or negative) and magnitude in the period after observations. The efficiency of biogenic carbon export into deeper water layers ranges from similar to 650 <(C:Fe)(export)

AB - The major response to ocean iron fertilization is by large diatoms, which at Fe-replete ambient seawater show an optimum C:Fe elemental ratio of similar to 23 000 and a higher ratio of similar to 160 000 or more under Fe-limited conditions. The efficiency of CO2 drawdown during the several weeks of artificial fertilization experiments with concomitant observations is in the range of 100 <(CO2:Fe) <1000 and is unknown in direction (positive or negative) and magnitude in the period after observations. The efficiency of biogenic carbon export into deeper water layers ranges from similar to 650 <(C:Fe)(export)

KW - iron

KW - fertilization

KW - ocean

KW - efficiency

KW - carbon

KW - export

KW - diatoms

KW - SOUTHERN-OCEAN

KW - PHYTOPLANKTON BLOOM

KW - MARINE-PHYTOPLANKTON

KW - ROSS SEA

KW - ENRICHMENT EXPERIMENT

KW - NORTHEAST PACIFIC

KW - LIGHT LIMITATION

KW - EXPERIMENT SOFEX

KW - ATLANTIC-OCEAN

KW - DISSOLVED IRON

U2 - 10.3354/meps07548

DO - 10.3354/meps07548

M3 - Article

VL - 364

SP - 269

EP - 282

JO - Marine Ecology Progress Series

JF - Marine Ecology Progress Series

SN - 0171-8630

ER -

ID: 1796956