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      Linking extracellular enzymes to phylogeny indicates a predominantly particle-associated lifestyle of deep-sea prokaryotes

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          Abstract

          Dominance of dissolved extracellular enzymes indicates that deep-sea prokaryotes are associated mainly with particulate matter.

          Abstract

          Heterotrophic prokaryotes express extracellular hydrolytic enzymes to cleave large organic molecules before taking up the hydrolyzed products. According to foraging theory, extracellular enzymes should be cell associated in dilute systems such as deep sea habitats, but secreted into the surrounding medium in diffusion-limited systems. However, extracellular enzymes in the deep sea are found mainly dissolved in ambient water rather than cell associated. In order to resolve this paradox, we conducted a global survey of peptidases and carbohydrate-active enzymes (CAZymes), two key enzyme groups initiating organic matter assimilation, in an integrated metagenomics, metatranscriptomics, and metaproteomics approach. The abundance, percentage, and diversity of genes encoding secretory processes, i.e., dissolved enzymes, consistently increased from epipelagic to bathypelagic waters, indicating that organic matter cleavage, and hence prokaryotic metabolism, is mediated mainly by particle-associated prokaryotes releasing their extracellular enzymes into diffusion-limited particles in the bathypelagic realm.

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          Intense hydrolytic enzyme activity on marine aggregates and implications for rapid particle dissolution

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            Bulk chemical characteristics of dissolved organic matter in the ocean.

            Dissolved organic matter (DOM) is the largest reservoir of reduced carbon in the oceans. The nature of DOM is poorly understood, in part, because it has been difficult to isolate sufficient amounts of representative material for analysis. Tangential-flow ultrafiltration was shown to recover milligram amounts of >1000 daltons of DOM from seawater collected at three depths in the North Pacific Ocean. These isolates represented 22 to 33 percent of the total DOM and included essentially all colloidal material. The elemental, carbohydrate, and carbon-type (by (13)C nuclear magnetic resonance) compositions of the isolates indicated that the relative abundance of polysaccharides was high ( approximately 50 percent) in surface water and decreased to approximately 25 percent in deeper samples. Polysaccharides thus appear to be more abundant and reactive components of seawater DOM than has been recognized.
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              Multi-faceted particle pumps drive carbon sequestration in the ocean

              The ocean's ability to sequester carbon away from the atmosphere exerts an important control on global climate. The biological pump drives carbon storage in the deep ocean and is thought to function via gravitational settling of organic particles from surface waters. However, the settling flux alone is often insufficient to balance mesopelagic carbon budgets or to meet the demands of subsurface biota. Here we review additional biological and physical mechanisms that inject suspended and sinking particles to depth. We propose that these 'particle injection pumps' probably sequester as much carbon as the gravitational pump, helping to close the carbon budget and motivating further investigation into their environmental control.
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                Author and article information

                Journal
                Sci Adv
                Sci Adv
                SciAdv
                advances
                Science Advances
                American Association for the Advancement of Science
                2375-2548
                April 2020
                15 April 2020
                : 6
                : 16
                : eaaz4354
                Affiliations
                [1 ]Department of Limnology and Bio-Oceanography, Center of Functional Ecology, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria.
                [2 ]NIOZ, Department of Marine Microbiology and Biogeochemistry, Royal Netherlands Institute for Sea Research, Utrecht University, AB Den Burg, Netherlands.
                [3 ]Vienna Metabolomics Center, University of Vienna, Althanstrasse, 14, A-1090 Vienna, Austria.
                Author notes
                [* ]Corresponding author. Email: gerhard.herndl@ 123456univie.ac.at
                Author information
                http://orcid.org/0000-0001-7497-3276
                http://orcid.org/0000-0001-8907-1494
                http://orcid.org/0000-0002-2223-2852
                Article
                aaz4354
                10.1126/sciadv.aaz4354
                7159927
                32494615
                a571a40c-460c-431d-8517-ce026c3613bf
                Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

                This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial license, which permits use, distribution, and reproduction in any medium, so long as the resultant use is not for commercial advantage and provided the original work is properly cited.

                History
                : 09 September 2019
                : 22 January 2020
                Categories
                Research Article
                Research Articles
                SciAdv r-articles
                Oceanography
                Oceanography
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                Nielsen Marquez

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