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      Negative CO 2 emissions via enhanced silicate weathering in coastal environments

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          Abstract

          Negative emission technologies (NETs) target the removal of carbon dioxide (CO 2) from the atmosphere, and are being actively investigated as a strategy to limit global warming to within the 1.5–2°C targets of the 2015 UN climate agreement. Enhanced silicate weathering (ESW) proposes to exploit the natural process of mineral weathering for the removal of CO 2 from the atmosphere. Here, we discuss the potential of applying ESW in coastal environments as a climate change mitigation option. By deliberately introducing fast-weathering silicate minerals onto coastal sediments, alkalinity is released into the overlying waters, thus creating a coastal CO 2 sink. Compared with other NETs, coastal ESW has the advantage that it counteracts ocean acidification, does not interfere with terrestrial land use and can be directly integrated into existing coastal management programmes with existing (dredging) technology. Yet presently, the concept is still at an early stage, and so two major research challenges relate to the efficiency and environmental impact of ESW. Dedicated experiments are needed (i) to more precisely determine the weathering rate under in situ conditions within the seabed and (ii) to evaluate the ecosystem impacts—both positive and negative—from the released weathering products.

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          Biophysical and economic limits to negative CO2 emissions

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            Bioturbation: a fresh look at Darwin's last idea.

            Bioturbation refers to the biological reworking of soils and sediments, and its importance for soil processes and geomorphology was first realised by Charles Darwin, who devoted his last scientific book to the subject. Here, we review some new insights into the evolutionary and ecological role of bioturbation that would have probably amazed Darwin. In modern ecological theory, bioturbation is now recognised as an archetypal example of 'ecosystem engineering', modifying geochemical gradients, redistributing food resources, viruses, bacteria, resting stages and eggs. From an evolutionary perspective, recent investigations provide evidence that bioturbation had a key role in the evolution of metazoan life at the end of the Precambrian Era.
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              Filamentous bacteria transport electrons over centimetre distances.

              Oxygen consumption in marine sediments is often coupled to the oxidation of sulphide generated by degradation of organic matter in deeper, oxygen-free layers. Geochemical observations have shown that this coupling can be mediated by electric currents carried by unidentified electron transporters across centimetre-wide zones. Here we present evidence that the native conductors are long, filamentous bacteria. They abounded in sediment zones with electric currents and along their length they contained strings with distinct properties in accordance with a function as electron transporters. Living, electrical cables add a new dimension to the understanding of interactions in nature and may find use in technology development.
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                Author and article information

                Journal
                Biol Lett
                Biol. Lett
                RSBL
                roybiolett
                Biology Letters
                The Royal Society
                1744-9561
                1744-957X
                April 2017
                5 April 2017
                5 April 2017
                : 13
                : 4
                : 20160905
                Affiliations
                [1 ]Department of Analytical, Environmental and Geo-Chemistry, Vrije Universiteit Brussel , Pleinlaan 2, 1050 Brussels, Belgium
                [2 ]Aarhus Institute of Advanced Studies (AIAS), Aarhus University , Hoegh-Guldbergs Gade 6B, 8000 Aarhus C, Denmark
                Author notes
                [†]

                Present address: Department of Marine Ecology, Management and Conservation, Institute for Oceanography—University of São Paulo (IO-USP), Praça do Oceanográfico 191, 05508-120, São Paulo, Brazil.

                An invited contribution to the mini-series ‘Enhanced rock weathering’ edited by David Beerling.

                Author information
                http://orcid.org/0000-0001-5334-7655
                Article
                rsbl20160905
                10.1098/rsbl.2016.0905
                5414690
                28381634
                92b122d1-3321-4b82-a08b-c8267090e114
                © 2017 The Authors.

                Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

                History
                : 21 December 2016
                : 28 January 2017
                Funding
                Funded by: European Research Council, http://dx.doi.org/10.13039/501100000781;
                Award ID: ERC Grant 306933
                Categories
                1001
                69
                Mini-Series
                Enhanced Rock Weathering
                Custom metadata
                April, 2017

                Life sciences
                climate change,carbon dioxide removal,enhanced weathering,olivine,marine ecosystems
                Life sciences
                climate change, carbon dioxide removal, enhanced weathering, olivine, marine ecosystems

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