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Evaluating the Potential Impacts of the Diurnal Vertical Migration by Marine Organisms on Marine Biogeochemistry

Global biogeochemical cycles, 2018-11, Vol.32 (11), p.1622-1643

2018

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Consistent trophic amplification of marine biomass declines under climate change

Global change biology, 2019-01, Vol.25 (1), p.218-229

2019

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The Impact of Variable Phytoplankton Stoichiometry on Projections of Primary Production, Food Quality, and Carbon Uptake in the Global Ocean

Global biogeochemical cycles, 2018-04, Vol.32 (4), p.516-528

2018

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The impact of different external sources of iron on the global carbon cycle

Geophysical research letters, 2014-02, Vol.41 (3), p.920-926

2014

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Impact of intensifying nitrogen limitation on ocean net primary production is fingerprinted by nitrogen isotopes

Nature communications, 2021-10, Vol.12 (1), p.6214-9, Article 6214

2021

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Influence of diatom diversity on the ocean biological carbon pump

Nature geoscience, 2018-01, Vol.11 (1), p.27-37

2018

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Spatial and body‐size dependent response of marine pelagic communities to projected global climate change

Global change biology, 2015-01, Vol.21 (1), p.154-164

2015

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Intermittency in phytoplankton bloom triggered by modulations in vertical stability

Scientific reports, 2021-01, Vol.11 (1), p.1285-1285, Article 1285

2021

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Evaluation of CNRM Earth System Model, CNRM‐ESM2‐1: Role of Earth System Processes in Present‐Day and Future Climate

Journal of advances in modeling earth systems, 2019-12, Vol.11 (12), p.4182-4227

2019

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Major Impact of Dust Deposition on the Productivity of the Arabian Sea

Geophysical research letters, 2019-06, Vol.46 (12), p.6736-6744

2019

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How well do global ocean biogeochemistry models simulate dissolved iron distributions?

Global biogeochemical cycles, 2016-02, Vol.30 (2), p.149-174

2016

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Decarbonization of academic laboratories: On the trade-offs between CO2 emissions, spending, and research output

Cleaner environmental systems, 2024-03, Vol.12, p.100168, Article 100168

2024

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The carbon footprint of scientific visibility

Environmental research letters, 2022-12, Vol.17 (12), p.124008

2022

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Should we account for mesozooplankton reproduction and ontogenetic growth in biogeochemical modeling?

Theoretical ecology, 2021-12, Vol.14 (4), p.589-609

2021

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Emergent constraints on projections of declining primary production in the tropical oceans

Nature climate change, 2017-05, Vol.7 (5), p.355-358

2017

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Evaluating the importance of atmospheric and sedimentary iron sources to Southern Ocean biogeochemistry

Geophysical research letters, 2009-07, Vol.36 (13), p.L13601-n/a

2009

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Skillful Seasonal Forecast of Sargassum Proliferation in the Tropical Atlantic

Geophysical research letters, 2023-11, Vol.50 (21), p.n/a

2023

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Projected decreases in future marine export production: the role of the carbon flux through the upper ocean ecosystem

Biogeosciences, 2016-07, Vol.13 (13), p.4023-4047

2016

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Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6

Current climate change reports, 2020-09, Vol.6 (3), p.95-119

2020

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Biogeochemical Protocols and Diagnostics for the CMIP6 Ocean Model Intercomparison Project (OMIP)

Geoscientific Model Development, 2017-06, Vol.10 (6), p.2169-2199

2017

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Hydrothermal contribution to the oceanic dissolved iron inventory

Nature geoscience, 2010-04, Vol.3 (4), p.252-256

2010

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Modeling the impacts of atmospheric deposition of nitrogen and desert dust-derived phosphorus on nutrients and biological budgets of the Mediterranean Sea

Progress in oceanography, 2018-04, Vol.163, p.21-39

2018

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Prey Stoichiometry Drives Iron Recycling by Zooplankton in the Global Ocean

Frontiers in Marine Science, 2020-06, Vol.7

2020

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Evaluating the Potential Impacts of the Diurnal Vertical Migration by Marine Organisms on Marine Biogeochemistry

Consistent trophic amplification of marine biomass declines under climate change

The Impact of Variable Phytoplankton Stoichiometry on Projections of Primary Production, Food Quality, and Carbon Uptake in the Global Ocean

The impact of different external sources of iron on the global carbon cycle

Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections

Impact of intensifying nitrogen limitation on ocean net primary production is fingerprinted by nitrogen isotopes

Influence of diatom diversity on the ocean biological carbon pump

Spatial and body‐size dependent response of marine pelagic communities to projected global climate change

Intermittency in phytoplankton bloom triggered by modulations in vertical stability

Evaluation of CNRM Earth System Model, CNRM‐ESM2‐1: Role of Earth System Processes in Present‐Day and Future Climate

Major Impact of Dust Deposition on the Productivity of the Arabian Sea

How well do global ocean biogeochemistry models simulate dissolved iron distributions?

Decarbonization of academic laboratories: On the trade-offs between CO2 emissions, spending, and research output

The carbon footprint of scientific visibility

Should we account for mesozooplankton reproduction and ontogenetic growth in biogeochemical modeling?

Emergent constraints on projections of declining primary production in the tropical oceans

Evaluating the importance of atmospheric and sedimentary iron sources to Southern Ocean biogeochemistry

Skillful Seasonal Forecast of Sargassum Proliferation in the Tropical Atlantic

Projected decreases in future marine export production: the role of the carbon flux through the upper ocean ecosystem

Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6

Biogeochemical Protocols and Diagnostics for the CMIP6 Ocean Model Intercomparison Project (OMIP)

Hydrothermal contribution to the oceanic dissolved iron inventory

Modeling the impacts of atmospheric deposition of nitrogen and desert dust-derived phosphorus on nutrients and biological budgets of the Mediterranean Sea

Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms

Prey Stoichiometry Drives Iron Recycling by Zooplankton in the Global Ocean

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