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      Seafloor primary production in a changing Arctic Ocean

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          Abstract

          Phytoplankton and sea ice algae are traditionally considered to be the main primary producers in the Arctic Ocean. In this Perspective, we explore the importance of benthic primary producers (BPPs) encompassing microalgae, macroalgae, and seagrasses, which represent a poorly quantified source of Arctic marine primary production. Despite scarce observations, models predict that BPPs are widespread, colonizing ~3 million km 2 of the extensive Arctic coastal and shelf seas. Using a synthesis of published data and a novel model, we estimate that BPPs currently contribute ~77 Tg C y −1 of primary production to the Arctic, equivalent to ~20 to 35% of annual phytoplankton production. Macroalgae contribute ~43 Tg C y −1 , seagrasses contribute ~23 Tg C y −1 , and microalgae-dominated shelf habitats contribute ~11 to 16 Tg C y −1 . Since 2003, the Arctic seafloor area exposed to sunlight has increased by ~47,000 km 2 y −1 , expanding the realm of BPPs in a warming Arctic. Increased macrophyte abundance and productivity is expected along Arctic coastlines with continued ocean warming and sea ice loss. However, microalgal benthic primary production has increased in only a few shelf regions despite substantial sea ice loss over the past 20 y, as higher solar irradiance in the ice-free ocean is counterbalanced by reduced water transparency. This suggests complex impacts of climate change on Arctic light availability and marine primary production. Despite significant knowledge gaps on Arctic BPPs, their widespread presence and obvious contribution to coastal and shelf ecosystem production call for further investigation and for their inclusion in Arctic ecosystem models and carbon budgets.

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          Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems.

          The cycles of the key nutrient elements nitrogen (N) and phosphorus (P) have been massively altered by anthropogenic activities. Thus, it is essential to understand how photosynthetic production across diverse ecosystems is, or is not, limited by N and P. Via a large-scale meta-analysis of experimental enrichments, we show that P limitation is equally strong across these major habitats and that N and P limitation are equivalent within both terrestrial and freshwater systems. Furthermore, simultaneous N and P enrichment produces strongly positive synergistic responses in all three environments. Thus, contrary to some prevailing paradigms, freshwater, marine and terrestrial ecosystems are surprisingly similar in terms of N and P limitation.
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            Marine Ecoregions of the World: A Bioregionalization of Coastal and Shelf Areas

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              Substantial role of macroalgae in marine carbon sequestration

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                Author and article information

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                Journal
                Proceedings of the National Academy of Sciences
                Proc. Natl. Acad. Sci. U.S.A.
                0027-8424
                1091-6490
                March 12 2024
                March 04 2024
                March 12 2024
                : 121
                : 11
                Affiliations
                [1 ]Department of Biology, University of Southern Denmark, 5230 Odense M, Denmark
                [2 ]Danish Institute for Advanced Study, University of Southern Denmark, 5230 Odense M, Denmark
                [3 ]Takuvik International Research Laboratory, CNRS/Université Laval, Québec City, QC G1V 0A6, Canada
                [4 ]Department of Biology, Chemistry and Geography, Université du Québec à Rimouski, Rimouski, QC G5L 3A1, Canada
                [5 ]Center for Remote Imaging, Sensing and Processing, National University of Singapore, Singapore 119076, Singapore
                [6 ]CNRS-Sorbonne Université, Laboratoire d’Océanographie, Villefranche-sur-Mer 06230, France
                [7 ]Institute for Sustainable Development and International Relations, Paris 75337, France
                [8 ]Benthic Communities Group/Institute of Marine Research, His 4817, Norway
                [9 ]School of Biological Science and Indian Oceans Marine Research Centre, University of Western Australia, Perth 6009, WA, Australia
                [10 ]Department of Ecoscience, Aarhus University, 8000 Aarhus C, Denmark
                [11 ]Arctic Research Center, Department of Biology, Aarhus University, 8000 Aarhus C, Denmark
                [12 ]Department of Biology, Marine Biological Section, University of Copenhagen, 3000 Helsingør, Denmark
                [13 ]ArcticNet, Department of Biology, Université Laval, Québec City, QC G1V 0A6, Canada
                [14 ]Department of Environmental Sciences, University of Virginia, Charlottesville, VA 400123
                [15 ]Department of Ocean and Environmental Sciences, Tokyo University of Marine Science and Technology, 108-8477 Tokyo, Japan
                [16 ]Norwegian Institute for Water Research, 0579 Oslo, Norway
                [17 ]Department of Mathematics and Computer Science, University of Southern Denmark, Odense, Denmark
                [18 ]Centre for Earth Observation Science, Clayton H. Riddell Faculty of Environment Earth, and Resources, University of Manitoba, Winnipeg, MB R3T 2N2, Canada
                [19 ]Helmholtz - Max Planck Joint Research Group for Deep Sea Ecology and Technology, Alfred-Wegener-Institute Helmholtz-Centre for Polar and Marine Research, Bremerhaven 27515, Germany
                [20 ]Helmholtz - Max Planck Joint Research Group for Deep Sea Ecology and Technology, Max-Planck-Institute for Marine Microbiology, Bremen 28359, Germany
                Article
                10.1073/pnas.2303366121
                6e42d18b-7dcc-4371-aaf6-e53ec9e3cdad
                © 2024

                https://creativecommons.org/licenses/by-nc-nd/4.0/

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