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From:PLoS ONE (Vol. 9, Issue 3) Peer-ReviewedAuthor(s): Joana Barcelos e Ramos 1,*, Kai Georg Schulz 2, Colin Brownlee 3, Scarlett Sett 4, Eduardo Brito Azevedo 1 Introduction Amongst the most recent (180 Ma [1]) planktonic unicellular autotrophs of Earth's...
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From:Marine Biology (Vol. 159, Issue 8) Peer-ReviewedThe flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes--remineralization rates and...
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From:Biogeosciences (Vol. 14, Issue 2) Peer-ReviewedCommunity approaches to investigating ocean acidification (OA) effects suggest a high tolerance of micro- and mesozooplankton to carbonate chemistry changes expected to occur within this century. Plankton communities in...
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From:Biogeosciences (Vol. 13, Issue 10) Peer-ReviewedStudies investigating the effect of increasing CO.sub.2 levels on the phosphorus cycle in natural waters are lacking although phosphorus often controls phytoplankton development in many aquatic systems. The aim of our...
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From:Biogeosciences (Vol. 13, Issue 13) Peer-ReviewedNitrogen fixation by filamentous cyanobacteria supplies significant amounts of new nitrogen (N) to the Baltic Sea. This balances N loss processes such as denitrification and anammox, and forms an important N source...
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From:Biogeosciences (Vol. 17, Issue 19) Peer-ReviewedEastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The production of organic material is fueled by upwelling of nutrient-rich deep waters and high incident light at the...