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      Response of a Coastal Microbial Community to Olivine Addition in the Muping Marine Ranch, Yantai

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          Abstract

          Spreading olivine powder in seawater to enhance alkalinity through weathering reactions has been proposed as a potential solution to control atmospheric CO 2 concentration. Attention has usually been paid to the chemical properties of seawater after the addition of olivine within lab and modeling studies. However, both microbial acclimation and evolution in such manipulated natural environments are often overlooked, yet they are of great importance for understanding the biological consequences of whether olivine addition is a feasible approach to mitigating climate change. In this study, an olivine addition experiment was conducted to investigate variation in bacterial diversity and community composition in the surface and bottom seawater of a representative marine ranch area in the Muping, Yantai. The results show that the composition of the particle-attached microbial community was particularly affected by the application of olivine. The relative abundance of biofilm-forming microbes in particle-attached fraction increased after the addition of olivine, while no significant variation in the free-living bacterial community was observed. Our study suggests that olivine addition would reshape the bacterial community structure, especially in particle-attached microenvironments. Therefore, the risk evaluation of alkalinity enhancement should be further studied before its large-scale application as a potential ocean geoengineering plan.

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            The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years

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              Paris Agreement climate proposals need a boost to keep warming well below 2 °C.

              The Paris climate agreement aims at holding global warming to well below 2 degrees Celsius and to "pursue efforts" to limit it to 1.5 degrees Celsius. To accomplish this, countries have submitted Intended Nationally Determined Contributions (INDCs) outlining their post-2020 climate action. Here we assess the effect of current INDCs on reducing aggregate greenhouse gas emissions, its implications for achieving the temperature objective of the Paris climate agreement, and potential options for overachievement. The INDCs collectively lower greenhouse gas emissions compared to where current policies stand, but still imply a median warming of 2.6-3.1 degrees Celsius by 2100. More can be achieved, because the agreement stipulates that targets for reducing greenhouse gas emissions are strengthened over time, both in ambition and scope. Substantial enhancement or over-delivery on current INDCs by additional national, sub-national and non-state actions is required to maintain a reasonable chance of meeting the target of keeping warming well below 2 degrees Celsius.
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                Author and article information

                Contributors
                Journal
                Front Microbiol
                Front Microbiol
                Front. Microbiol.
                Frontiers in Microbiology
                Frontiers Media S.A.
                1664-302X
                10 February 2022
                2021
                : 12
                : 805361
                Affiliations
                [1] 1Institute of Marine Science and Technology, Shandong University , Qingdao, China
                [2] 2Joint Laboratory for Ocean Research and Education at Dalhousie University, Shandong University , Qingdao, China
                [3] 3Joint Laboratory for Ocean Research and Education at Dalhousie University, Xiamen University , Xiamen, China
                [4] 4Southern Marine Science and Engineering Guangdong Laboratory , Zhuhai, China
                [5] 5School of Earth Science and Resources, Chang’an University , Xi’an, China
                [6] 6College of Geology and Environment, Xi’an University of Science and Technology , Xi’an, China
                [7] 7Institute of Marine Microbes and Ecospheres, Xiamen University , Xiamen, China
                [8] 8State Key Laboratory of Marine Environmental Science and College of Ocean and Earth Sciences, Fujian Key Laboratory of Marine Carbon Sequestration, Xiamen University , Xiamen, China
                [9] 9Key Laboratory of Tropical Marine Bio-Resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences , Guangzhou, China
                Author notes

                Edited by: Yuanyuan Feng, Shanghai Jiao Tong University, China

                Reviewed by: Ye Deng, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences (CAS), China; Renmao Tian, Illinois Institute of Technology, United States

                *Correspondence: Yubin Hu, yubinhu@ 123456sdu.edu.cn

                This article was submitted to Aquatic Microbiology, a section of the journal Frontiers in Microbiology

                Article
                10.3389/fmicb.2021.805361
                8867022
                3512e1dd-4240-4fbc-bce9-6c2e1d3548cd
                Copyright © 2022 Ren, Hu, Liu, Zhang, Mou, Pan, Zheng, Li and Jiao.

                This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

                History
                : 30 October 2021
                : 06 December 2021
                Page count
                Figures: 6, Tables: 0, Equations: 0, References: 52, Pages: 10, Words: 6190
                Categories
                Microbiology
                Original Research

                Microbiology & Virology
                co2 sequestration,silicate mineral dissolution,seawater alkalinity,enhanced weathering,bacterial community

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