Biogeochemical fluxes through mesozooplankton

By E. Buitenhuis, Corinne Le Quéré, O. Aumont, Grégory Beaugrand, Adrian Bunker, A. Hirst, T. Ikeda, T. O’Brien, S. Piontkovski, D. Straile. 2006

226 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/89d07eae4cc9d56c93bb685127952a4c01a3eb01

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. E. Buitenhuis
2. T. Hashioka
3. M. Ohman
4. S. Doney
5. Corinne Le Quéré
6. C. Trueman
7. B. Houlton
8. K. Eiane

In Oceanography

1. S. Doney
2. I. Lima
3. C. Cleveland
4. E. Buitenhuis
5. T. Hashioka
6. Thomas R. Anderson
7. M. Ohman
8. R. Lampitt

Citations in the corpus

• Multi-element regulation of the tropical forest carbon cycle (2011, methodology): “…production data using data from the Carbon Dioxide Information Analysis Center, and removed ocean fluxes from atmospheric observations using the Le Quéré et al. (2007) Ocean Parallelise (OPA) General Circulation Model, coupled to the PISCES-T biogeochemistry model of Buitenhuis et al. (2006).”
• Contributions of mesozooplankton to vertical carbon export in a coastal upwelling system (2013, background): “…phytoplankton produc- tion, aggregation (Alldredge & Gotschalk 1989, Jackson et al. 2005), mineral ballasting (Armstrong et al. 2001), and mesozooplankton grazing (Buitenhuis et al. 2006) to vertical carbon flux are still hotly debated and likely to vary spatially and temporally (Burd et al. 2010).”
• Combined constraints on global ocean primary production using observations and models (2013, background): “…of primary production that is exuded as dissolved organic carbon (DOC), PPi e is the assimilation rate of phytoplankton (equations (2), (4), and (5)), wPi is the total loss rate (equation (6)), and gZj Pi is the grazing rate of zooplankton Zj on phytoplankton Pi [Buitenhuis et al., 2006, 2010].”
• Phytoplankton competition during the spring bloom in four Plankton Functional Type Models (2012, result): “These properties are consistent with observational studies for microzooplankton (Buitenhuis et al., 2010); mesozooplankton (Buitenhuis et al., 2006) and macrozooplankton (Moriarty, 2009).”
• Quantifying carbon fluxes from primary production to mesopelagic fish using a simple food web model (2019, methodology): “Mesozooplankton grazing of between 19 and 11.2 Gt C year 1 was predicted using different versions of the PISCES model by Buitenhuis et al. (2006) and Aumont et al. (2015), respectively, which convert to fractions of PP of 0.27 and 0.25 (based on PP of 69.7 vs. 44.3 Gt C year 1 for the two models).”