Trichodesmium physiological ecology and phosphate reduction in the western tropical South Pacific

Autor: K. R. Frischkorn, A. Krupke, C. Guieu, J. Louis, M. Rouco, A. E. Salazar Estrada, B. A. S. Van Mooy, S. T. Dyhrman

Publikováno v: Biogeosciences, Vol 15, Pp 5761-5778 (2018)

N2 fixation by the genus Trichodesmium is predicted to support a large proportion of the primary productivity across the oligotrophic oceans, regions that are considered among the largest biomes on Earth. Many of these environments remain poorly

Externí odkaz: https://doaj.org/article/ebe242962dae4dc8b939fc87bb964552

Phospholipid synthesis rates in the eastern subtropical South Pacific Ocean

Autor: B. A. S. Van Mooy, T. Moutin, S. Duhamel, P. Rimmelin, F. Van Wambeke

Publikováno v: Biogeosciences, Vol 5, Iss 1, Pp 133-139 (2008)

Membrane lipid molecules are a major component of planktonic organisms and this is particularly true of the microbial picoplankton that dominate the open ocean; with their high surface-area to volume ratios, the synthesis of membrane lipids places a

Externí odkaz: https://doaj.org/article/f8bb4df3f313407181f0f813cce07626

Major role of planktonic phosphate reduction in the marine phosphorus redox cycle

Autor: Justin E. Ossolinski, Sonya T. Dyhrman, Kyle R. Frischkorn, Mónica Rouco, Helen F. Fredricks, Andreas Krupke, Sean P. Sylva, J. D. Seewald, B. A. S. Van Mooy, Daniel J. Repeta

Publikováno v: Science. 348:783-785

Phosphorus in the +5 oxidation state (i.e., phosphate) is the most abundant form of phosphorus in the global ocean. An enigmatic pool of dissolved phosphonate molecules, with phosphorus in the +3 oxidation state, is also ubiquitous; however, cycling

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::60d2dfe1c18da6e3d974b343666cf65b
https://doi.org/10.1126/science.aaa8181

Phosphate availability and the ultimate control of new nitrogen input by nitrogen fixation in the tropical Pacific Ocean

Autor: Peggy Rimmelin, Thierry Moutin, B. A. S. Van Mooy, Solange Duhamel, Hervé Claustre, David M. Karl, Patrick Raimbault

Publikováno v: Biogeosciences, Vol 5, Iss 1, Pp 95-109 (2008)
Biogeosciences
Biogeosciences, European Geosciences Union, 2008, 5 (1), pp.95-109
Scopus-Elsevier
Biogeosciences Discussions
Biogeosciences Discussions, European Geosciences Union, 2007, 4 (4), pp.2407-2440
Biogeosciences, 2008, 5 (1), pp.95-109. ⟨10.5194/bg-5-95-2008⟩
Biogeosciences Discussions, 2007, 4 (4), pp.2407-2440

Due to the low atmospheric input of phosphate into the open ocean, it is one of the key nutrients that could ultimately control primary production and carbon export into the deep ocean. The observed trend over the last 20 years has shown a decrease i

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a3c2435a9924032741899c45a8b3a873
http://www.biogeosciences.net/5/95/2008/bg-5-95-2008.pdf

Gradients in intact polar diacylglycerolipids across the Mediterranean Sea are related to phosphate availability

Autor: Thierry Moutin, Claude Courties, L. E. Sofen, Louise Oriol, B. A. S. Van Mooy, Anna Lagaria, Mireille Pujo-Pay, Kimberly J. Popendorf, Tsuneo Tanaka, Pascal Conan

Publikováno v: Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2011, Vol. 8, N. 12, P. 3733-3745
Biogeosciences
Biogeosciences, European Geosciences Union, 2011, 8 (12), pp.3733-3745. 〈10.5194/bg-8-3733-2011〉
Biogeosciences, Vol 8, Iss 12, Pp 3733-3745 (2011)
Biogeosciences, 2011, 8 (12), pp.3733-3745. ⟨10.5194/bg-8-3733-2011⟩
Biogeosciences, European Geosciences Union, 2011, 8 (12), pp.3733-3745. ⟨10.5194/bg-8-3733-2011⟩
Biogeosciences, 2011, 8, pp.3733-3745. ⟨10.5194/bg-8-3733-201110.5194/bgd-8-7921-2011⟩

Intact polar membrane lipids compose a significant fraction of cellular material in plankton and their synthesis imposes a substantial constraint on planktonic nutrient requirements. As a part of the Biogeochemistry from the Oligotrophic to the Ultra

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::335c7f59113b7ebdb0bbc68535ced0c3
https://archimer.ifremer.fr/doc/00133/24405/