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  <doc index="1" percent="">
    <id>878471</id>
    <classid>1564</classid>
    <newstime>1771254952</newstime>
    <tbname>med24</tbname>
    <title>Microbe-Mediated Degradation of Polyethylene and Release of Associated Pollutants under Simulated Dark Environments</title>
    <autocomplete>polyethylene degradation,microbe-mediated,pollutant release</autocomplete>
    <citation>2026 Feb 12.</citation>
    <doi>10.1021/acs.est.5c16964</doi>
    <enabstracts>Polyethylene (PE) dominates global packaging waste, yet its fate remains poorly understood in dark, anoxic environments such as ocean sediments and landfills, which represent important reservoirs for discarded plastics. In this study, 800-day microcosm experiments were performed with PE samples retrieved from an active landfill site with distinct landfill durations. Results demonstrated that anaerobic microbes slowly degrade PE while enhancing the release of secondary pollutants, such as nanoplastics (NPs) and phthalate esters (PAEs). Microbial colonization increased the surface roughness of PE samples and the abundance of oxygenated functional groups, driving oxidative chain scission, NP release (2.4-4.3 × 1011 particles mL-1 leachate), and PAE biodegradation. Logarithmic curves derived from an improved Polymer Aging Index revealed a midage acceleration window, with PE buried for 7 years being the most susceptible to microbial attack. PE-associated microbial communities were dominated by deterministic assembly processes, with functional taxa being the dominant drivers of PE aging, and PAE degraders exhibiting dual-threshold dynamics. Together, this study identifies a coupled oxidation-biodegradation-fragmentation feedbacks mechanism that governs the fate of PE in landfills, highlighting the dual microbial role in degrading PE and amplifying associated pollutant release.                                                                                                                  Keywords:                    assembly mechanism; degradation bacteria; landfill leachate; microorganisms; microplastic.</enabstracts>
    <journal2>Environ Sci Technol</journal2>
    <issn>1520-5851</issn>
    <affiliations>1 School of Environmental Science and Engineering, Shanghai Engineering Research Center of Solid Waste Treatment, Shanghai Jiao Tong University, Shanghai 200240, China.2 Chinese Research Academy of Environmental Sciences, Beijing 100012, China.3 College of Environmental and Resources Sciences, Zhejiang University, Hangzhou 310058, China.4 School of Resources and Environmental Engineering, Anhui University, Hefei 230601, China.5 China School of Resource Environment and Safety Engineering, University of South China, Hengyang 421001, China.6 College of Environmental Science and Engineering, Central South University of Forestry and Technology, Changsha 410004, China.</affiliations>
    <journal><![CDATA[Environmental science & technology]]></journal>
    <writer>Yang C;Huang Q;Wang H;Xue Z;Lin X;Song L;Cheng Z;Yuan Z;Yuan H;Zhu N;Kong L;Lou Z;</writer>
    <author1>Changfu Yang,Qiujie Huang,Hui Wang,Zhirong Xue,Xiaoxing Lin,Liyan Song,Zhaowen Cheng,Zhihang Yuan,Haiping Yuan,Nanwen Zhu,Long Kong,Ziyang Lou</author1>
    <author><![CDATA[Changfu Yang&nbsp; 1,&nbsp;Qiujie Huang&nbsp; 1&nbsp; 2,&nbsp;Hui Wang&nbsp; 1,&nbsp;Zhirong Xue&nbsp; 1,&nbsp;Xiaoxing Lin&nbsp; 3,&nbsp;Liyan Song&nbsp; 4,&nbsp;Zhaowen Cheng&nbsp; 5,&nbsp;Zhihang Yuan&nbsp; 6,&nbsp;Haiping Yuan&nbsp; 1,&nbsp;Nanwen Zhu&nbsp; 1,&nbsp;Long Kong&nbsp; 1,&nbsp;Ziyang Lou&nbsp; 1]]></author>
    <date>2026</date>
    <ftitle>模拟暗环境中微生物介导的聚乙烯降解及关联污染物的释放</ftitle>
    <pmid>41684061</pmid>
    <keywordcn>聚乙烯降解,微生物介导,污染物释放</keywordcn>
  </doc>
  <doc index="2" percent="">
    <id>675806</id>
    <classid>1557</classid>
    <newstime>1767701059</newstime>
    <tbname>med24</tbname>
    <title>Purifying selection and low recombination facilitated sequential colonization of benthic and pelagic coastal ocean by ammonia-oxidizing archaea</title>
    <autocomplete>Purifying selection and low recombination facilitated sequential colonization of benthic and pelagic coastal ocean by ammonia-oxidizing archaea</autocomplete>
    <citation>2025 Dec 8;5(1):ycaf234.</citation>
    <doi>10.1093/ismeco/ycaf234</doi>
    <enabstracts>The evolutionary adaptation of archaea to ecologically diverse habitats remains poorly understood. Ammonia-oxidizing archaea (AOA) exhibit significant diversification across various environmental conditions; however, their ecological dynamics, diversification, and associated evolutionary processes are still largely unexplored in coastal environments, which contain extensive ecosystem heterogeneity. Combining newly assembled metagenomic data from Chinese marginal seas (2059 km coverage) with global datasets (spanning over 16 000 km), these knowledge gaps were explored across a continental-scale latitudinal gradient. It revealed that coastal AOA genomic diversity is latitude-dependent, with predicted optimum growth temperatures and substrate metabolic pathways explaining the geographical distribution. The two dominant genus-level clades exhibited significantly distinct benthic-pelagic niches, associated with specific genes involved in nutrient uptake and stress resistance. Phylogenomic reconstructions suggest that AOA initially colonized the coastal ocean sediments around 718 million years ago (Mya), and subsequent purifying selection and low recombination facilitated the AOA niche expansion into marine coastal environments. By revealing the evolutionary trajectories of Nitrososphaeria and their differential colonization patterns, our findings offer a novel perspective on the mechanisms of AOA diversification in the coastal ocean. This work advances our understanding of microbial diversification and niche differentiation of AOA in coastal ecosystems as well as the evolutionary forces shaping their global biogeography.                                                                                                                  Keywords:                    Nitrososphaeria; ammonia-oxidizing archaea; coastal ocean; evolutionary adaptation; niche transition.                      © The Author(s) 2025. Published by Oxford University Press on behalf of the International Society for Microbial Ecology.</enabstracts>
    <journal2>ISME Commun</journal2>
    <issn>2730-6151</issn>
    <affiliations><![CDATA[1 Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China.2 Laboratory for Marine Ecology and Environmental Science, Qingdao Marine Science and Technology Center, Qingdao 266237, China.3 Key Laboratory of Evolution & Marine Biodiversity (Ministry of Education) and Institute of Evolution & Marine Biodiversity, Ocean University of China, Qingdao 266003, China.4 School of Biological Sciences, University of Aberdeen, Aberdeen AB24 3UU, United Kingdom.]]></affiliations>
    <journal>ISME communications</journal>
    <writer>Ren G;Gubry-Rangin C;Wang W;Liu R;Liu J;Liu J;Zhang XH;Liu J;</writer>
    <author1>Gaoyang Ren,Cécile Gubry-Rangin,Wenhao Wang,Ronghua Liu,Jiao Liu,Jinmei Liu,Xiao-Hua Zhang,Jiwen Liu</author1>
    <author><![CDATA[Gaoyang Ren&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Cécile Gubry-Rangin&nbsp; 4,&nbsp;Wenhao Wang&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Ronghua Liu&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Jiao Liu&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Jinmei Liu&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Xiao-Hua Zhang&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Jiwen Liu&nbsp; 1&nbsp; 2&nbsp; 3]]></author>
    <date>2025</date>
    <pmid>41480265</pmid>
    <ftitle>纯化选择和低重组使氨氧化古菌依次定植滨海海底和水柱环境</ftitle>
    <keyboard>purifying selection,recombination,colonization,ammonia-oxidizing archaea</keyboard>
    <keywordcn>净化选择,重组,定植,氨氧化古菌</keywordcn>
  </doc>
  <doc index="3" percent="">
    <id>401227</id>
    <classid>1548</classid>
    <newstime>1762754364</newstime>
    <tbname>med24</tbname>
    <title>Quantifying the Denticle Multiverse: A Standardized Coding System to Capture Three Dimensional Morphological Variations for Quantitative Evolutionary and Ecological Studies of Elasmobranch Denticles</title>
    <autocomplete>elasmobranch denticles,standardized coding system,three dimensional morphology</autocomplete>
    <citation>2025 May 13;7(1):obaf021.</citation>
    <doi>10.1093/iob/obaf021</doi>
    <enabstracts>Dermal denticles-microscopic tooth-like scales-are a major defining feature of elasmobranch skin, and are of interest to a wide array of fields, including paleontology, evolutionary biology, developmental biology, functional morphology, and bio-inspired design. While dermal denticle research is a growing field, there is currently no standardized vocabulary or framework to compare denticle morphology across research fields, siloing, and limiting denticle research efforts. Here, we present a morphological framework, which includes a character code that comprehensively captures denticle morphology from a wide diversity of denticle sampling types and imaging methods, and is backed by an easy-to-use google sheets-based coding tool and R package for replicating disparity analyses. The code is based on a wide-spread literature review of published denticle images, scanning electron microscope (SEMs), and computed tomography (CT) scans of extant shark denticles, and a review of tens of thousands of fossil denticles from pelagic ocean sediments dating back over 100 million years. The code's flexibility and replicability facilitate comparison across studies and independent research teams, and the addition of novel character categories. Denticle morphotypes are defined as denticles with unique combinations of character traits. This coding system facilitates morphologically backed disparity analyses of denticle morphological diversity, whether through deep time, across the body of a shark, or across a time-series of development, providing a more detailed, quantitative, and universal tool for analyzing denticle morphology across studies.                                                                                                                                        Dentículos dérmicos - escamas microscópicas semelhantes a dentes - são uma característica diagnostica importante da pele dos elasmobrânquios e são de interesse para uma ampla variedade de áreas, incluindo paleontologia, biologia evolutiva, biologia do desenvolvimento, morfologia funcional e design bioinspirado. Embora a pesquisa sobre dentículos dérmicos seja uma área em crescimento, atualmente não existe um vocabulário ou estrutura padronizada para comparar a morfologia dos dentículos entre diferentes áreas de pesquisa, o que acaba isolando e limitando os esforços de pesquisa sobre dentículos. Aqui, apresentamos uma estrutura morfológica que inclui um código de caracteres que captura de maneira abrangente a morfologia dos dentículos a partir de uma grande diversidade de tipos de amostras de dentículos e métodos de imagem, e que é respaldada por uma ferramenta de codificação fácil de usar baseada no Google Sheets e por um pacote R para replicar análises de disparidade. O código é baseado em uma ampla revisão da literatura de imagens publicadas de dentículos, MEVs e tomografias computadorizadas (CT) de dentículos de tubarões viventes, além de uma revisão de dezenas de milhares de dentículos fósseis de sedimentos oceânicos pelágicos com mais de 100 milhões de anos. A flexibilidade e replicabilidade do código facilitam a comparação entre estudos e equipes de pesquisa independentes, além da adição de novas categorias de caracteres. Os morfotipos de dentículos são definidos como dentículos com combinações únicas de características. Este sistema de codificação facilita análises de disparidade com base morfológica sobre a diversidade morfológica dos dentículos, seja ao longo do tempo geológico, ao longo do corpo de um tubarão, ou ao longo de uma série temporal de desenvolvimento, oferecendo uma ferramenta mais detalhada, quantitativa e universal para analisar a morfologia dos dentículos em diferentes estudos.                                                                                                                                        Cuantificación del multiverso de dentículos: Un sistema de codificación estandarizado para capturar la variación morfológica tridimensional para estudios cuantitativos evolutivos y ecológicos de dentículos dérmicos de elasmobranquios.Los dentículos dérmicos (escamas microscópicas similares a dientes) son una característica definitoria importante de la piel de los elasmobranquios y son de interés para una amplia gama de campos, incluyendo la paleontología, la biología evolutiva, la biología del desarrollo, la morfología funcional y la ingeniería biomimética. Mientras la investigación de los dentículos dérmicos es un campo en expansión, actualmente no existe un vocabulario ni un marco estandarizado para comparar la morfología de los dentículos en diferentes campos de estudio, lo que aísla y limita los esfuerzos de investigación. Aquí se presenta un marco morfológico que incluye un código de caracteres que captura exhaustivamente la morfología de los dentículos dérmicos a partir de una amplia diversidad de tipos de muestreo y métodos de imagen. Este marco está respaldado por una herramienta de codificación fácil de usar basada en hojas de cálculo de Google y un paquete R para replicar análisis de disparidad. El código se basa en una extensa revisión bibliográfica de imágenes publicadas, microscopía electrónica de barrido (MEB) y tomografías computarizadas de dentículos de tiburón existentes, y en una revisión de decenas de miles de dentículos fósiles de sedimentos oceánicos pelágicos que datan de más de 100 millones de años. La flexibilidad y replicabilidad del código facilitan la comparación entre estudios y equipos de investigación independientes, así como la incorporación de nuevas categorías de caracteres. Los morfotipos de dentículos se definen como dentículos que presentan combinaciones únicas de rasgos de carácter. Este sistema de codificación facilita el análisis de disparidad morfológica de la diversidad de los dentículos, ya sea a lo largo de grandes períodos de tiempo, a lo largo del cuerpo de un tiburón o a lo largo de una serie temporal de desarrollo, proporcionando una herramienta más detallada, cuantitativa y universal para el análisis de la morfología de los dentículos dérmicos en diferentes estudios.                                                                                        © The Author(s) 2025. Published by Oxford University Press on behalf of the Society for Integrative and Comparative Biology.</enabstracts>
    <journal2>Integr Org Biol</journal2>
    <issn>2517-4843</issn>
    <affiliations>1 Department of Environmental Biology, The State University of New York College of Environmental Science and Forestry, Syracuse, NY 13210, USA.2 Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.3 Department of Biology, University of Florida, Gainesville, FL 32611, USA.4 Museum of Comparative Zoology, Harvard University, Cambridge, MA 02138, USA.5 Brown University Department of Earth, Environment and Planetary Sciences, Providence, RI 02912, USA.6 Natural History Museum, London SW7 5BD, UK.</affiliations>
    <journal>Integrative organismal biology (Oxford, England)</journal>
    <writer>Rubin LD;Fraser GJ;Gabler-Smith MK;Lauder GV;Ribeiro WV;Vaz DFB;Wallis-Mauro N;Sibert EC;</writer>
    <author1>L D Rubin,G J Fraser,M K Gabler-Smith,G V Lauder,W V Ribeiro,D F B Vaz,N Wallis-Mauro,E C Sibert</author1>
    <author><![CDATA[L D Rubin&nbsp; 1&nbsp; 2,&nbsp;G J Fraser&nbsp; 3,&nbsp;M K Gabler-Smith&nbsp; 4,&nbsp;G V Lauder&nbsp; 4,&nbsp;W V Ribeiro&nbsp; 5,&nbsp;D F B Vaz&nbsp; 6,&nbsp;N Wallis-Mauro&nbsp; 2&nbsp; 3,&nbsp;E C Sibert&nbsp; 2]]></author>
    <date>2025</date>
    <ftitle>量化棘鳞多元宇宙：一个标准化编码系统，用于捕捉形态学变化的三维变异，以进行定量进化和生态研究的软骨鱼类棘鳞分类体系</ftitle>
    <pmid>41201038</pmid>
    <keywordcn>板鳃鱼鳞片,标准化编码系统,三维形态学</keywordcn>
  </doc>
  <doc index="4" percent="">
    <id>252690</id>
    <classid>1543</classid>
    <newstime>1759890898</newstime>
    <tbname>med24</tbname>
    <title>Spatial self-organization of confined bacterial suspensions</title>
    <autocomplete>Spatial self-organization of confined bacterial suspensions</autocomplete>
    <citation>2025 Oct 14;122(41):e2503983122.</citation>
    <doi>10.1073/pnas.2503983122</doi>
    <enabstracts>Lab studies of bacteria usually focus on cells in spatially extended, nutrient-replete settings, such as in liquid cultures and on agar surfaces. By contrast, many biological and environmental settings-ranging from mucus in the body to ocean sediments and the soil beneath our feet-feature multicellular bacterial populations that are confined to tight spots where essential metabolic substrates (e.g., oxygen) are scarce. What influence does such confinement have on a bacterial population? Here, we address this question by studying suspensions of motile Escherichia coli confined to quasi two-dimensional (2D) droplets. We find that when the droplet size and cell concentration are both large enough, the initially uniform suspension spatially self-organizes into a concentrated, immotile inner "core" that coexists with a more dilute, highly motile surrounding "shell." By simultaneously measuring cell concentration, oxygen concentration, and motility-generated fluid flow, we show that this behavior arises from the interplay between oxygen transport through the droplet from its boundary, uptake by the cells, and corresponding changes in their motility in response to oxygen variations. Furthermore, we use biophysical theory and simulations to quantitatively describe this interplay. Our work thus sheds light on the rich collective behaviors that emerge for bacterial populations in confined environments, with implications for understanding ecological niches and engineering artificial systems.                                                                                                                  Keywords:                    active matter; bacteria; pattern formation; reaction–diffusion; self-organization.</enabstracts>
    <journal2>Proc Natl Acad Sci U S A</journal2>
    <issn>1091-6490</issn>
    <affiliations>1 Department of Chemical and Biological Engineering, Princeton University, Princeton, NJ 08544.2 Princeton Center for Theoretical Science, Princeton University, Princeton, NJ 08544.3 Lewis-Sigler Institute for Integrative Genomics, Princeton University, Princeton, NJ 08540.4 Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125.</affiliations>
    <journal>Proceedings of the National Academy of Sciences of the United States of America</journal>
    <writer>Hokmabad BV;Martínez-Calvo A;Gonzalez La Corte S;Datta SS;</writer>
    <author1>Babak Vajdi Hokmabad,Alejandro Martínez-Calvo,Sebastian Gonzalez La Corte,Sujit S Datta</author1>
    <author><![CDATA[Babak Vajdi Hokmabad&nbsp; 1,&nbsp;Alejandro Martínez-Calvo&nbsp; 1&nbsp; 2,&nbsp;Sebastian Gonzalez La Corte&nbsp; 3,&nbsp;Sujit S Datta&nbsp; 1&nbsp; 4]]></author>
    <date>2025</date>
    <pmid>41052330</pmid>
    <ftitle>限制条件下细菌悬浮液的空间自组织行为研究</ftitle>
    <keyboard>spatial self-organization,bacterial suspensions</keyboard>
    <keywordcn>空间自组织,细菌悬浮液</keywordcn>
  </doc>
  <doc index="5" percent="">
    <id>138774</id>
    <classid>1539</classid>
    <newstime>1757922262</newstime>
    <tbname>med24</tbname>
    <title>Why Do Filamentous Actinomycetota Produce Such a Vast Array of Specialized Metabolites?</title>
    <autocomplete>Why Do Filamentous Actinomycetota Produce Such a Vast Array of Specialized Metabolites?</autocomplete>
    <citation>2025 Sep 12.</citation>
    <doi>10.1146/annurev-micro-060424-051257</doi>
    <enabstracts>Bacteria of the phylum Actinomycetota are extremely diverse: They inhabit niches ranging from soils and ocean sediments to the normal human microbiota, and they cause tuberculosis, one of the most prevalent chronic bacterial infections. They display an accordingly wide range of adaptive traits that enable their persistence, including, in some clades, a vast repertoire of biologically active small molecules. While humans have capitalized on this trove of useful natural products (also called secondary or specialized metabolites), the utility of these molecules for their producers has been challenging to directly assess. In this review, we consider adaptations that may have paved the way for the evolution of the expansive specialized metabolisms present in certain clades of Actinomycetota. We also consider the evolutionary pressures that may have driven diversification of these metabolisms and document how these organisms use these molecules in microbial interactions.</enabstracts>
    <journal2>Annu Rev Microbiol</journal2>
    <issn>1545-3251</issn>
    <affiliations>1 Department of Plant and Microbial Biology, University of California, Berkeley, California, USA ; email: mtrax@berkeley.edu.</affiliations>
    <journal>Annual review of microbiology</journal>
    <writer>Morin LMC;Dekoninck K;Sridhar V;Disney-McKeethen S;Proctor T;Eng AY;Traxler MF;</writer>
    <author1>Luis M Cantu Morin,Kilian Dekoninck,Varun Sridhar,Saoirse Disney-McKeethen,Theresa Proctor,Ashley Y Eng,Matthew F Traxler</author1>
    <author><![CDATA[Luis M Cantu Morin&nbsp; 1,&nbsp;Kilian Dekoninck&nbsp; 1,&nbsp;Varun Sridhar&nbsp; 1,&nbsp;Saoirse Disney-McKeethen&nbsp; 1,&nbsp;Theresa Proctor&nbsp; 1,&nbsp;Ashley Y Eng&nbsp; 1,&nbsp;Matthew F Traxler&nbsp; 1]]></author>
    <date>2025</date>
    <pmid>40939134</pmid>
    <pubtype>Review</pubtype>
    <ftitle>丝状放线菌为什么会产生如此众多的专业代谢产物？</ftitle>
    <keyboard>filamentous actinomycetota,specialized metabolites</keyboard>
    <keywordcn>丝状放线菌门,专业代谢物</keywordcn>
  </doc>
  <doc index="6" percent="">
    <id>1766775</id>
    <classid>548</classid>
    <newstime>1754613911</newstime>
    <tbname>med9</tbname>
    <title>A 12,800-year-old layer with cometary dust, microspherules, and platinum anomaly recorded in multiple cores from Baffin Bay</title>
    <autocomplete>cometary dust,microspherules,platinum anomaly</autocomplete>
    <citation>2025 Aug 6;20(8):e0328347.</citation>
    <doi>10.1371/journal.pone.0328347</doi>
    <enabstracts>The Younger Dryas Impact Hypothesis (YDIH) posits that ~12,800 years ago Earth encountered the debris stream of a disintegrating comet, triggering hemisphere-wide airbursts, atmospheric dust loading, and the deposition of a distinctive suite of extraterrestrial (ET) impact proxies at the Younger Dryas Boundary (YDB). Until now, evidence supporting this hypothesis has come only from terrestrial sediment and ice-core records. Here we report the first discovery of similar impact-related proxies in ocean sediments from four marine cores in Baffin Bay that span the YDB layer at water depths of 0.5-2.4 km, minimizing the potential for modern contamination. Using scanning electron microscopy with energy-dispersive spectroscopy (SEM-EDS) and laser ablation ICP-MS, we detect synchronous abundance peaks of metallic debris geochemically consistent with cometary dust, co-occurring with iron- and silica-rich microspherules (4-163 μm) that are predominantly of terrestrial origin with minor (</enabstracts>
    <journal2>PLoS One</journal2>
    <issn>1932-6203</issn>
    <affiliations>1 South Carolina Institute for Archaeology and Anthropology, University of South Carolina, Columbia, South Carolina, United States of America.2 South Carolina Department of Natural Resources, Heritage Trust Program; Land, Water, and Conservation Division, Columbia, South Carolina, United States of America.3 Borok Geophysical Observatory of Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences, Russian Federation.4 Center of Excellence in Remote Sensing Education and Research, Elizabeth City State University, Elizabeth City, North Carolina, United States of America.5 Comet Research Group, Prescott, Arizona, United States of America.6 Department of Earth, Environment and Planning, East Carolina University, Greenville, North Carolina, United States of America.7 Center for Environmental Nanoscience and Risk (CENR), Department of Environmental Health Sciences, Arnold School of Public Health, University of South Carolina, Columbia, United States of America.8 Department of Earth Science and Marine Science Institute, University of California Santa Barbara, Santa Barbara, California, United States of America.9 Armagh Observatory and Planetarium, College Hill, Armagh, Northern Ireland.10 School of Earth, Ocean and Environment, University of South Carolina, Columbia, South Carolina, United States of America.11 Department of Natural Sciences, Elizabeth City State University, Elizabeth City, North Carolina, United States of America.12 Department of Geoscience, University of Wisconsin - Madison, Madison, Wisconsin, United States of America.13 Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska, United States of America.14 Institute of Hydrogeology, Engineering Geology and Applied Geophysics, Charles University, Prague, Czechia.15 Center for Advanced Materials Characterization in Oregon, University of Oregon, Eugene, Oregon, United States of America.16 Electron Microscopy and Surface Analysis Lab, Nanofab, University of Utah, Salt Lake City, Utah, United States of America.17 College of Humanities, Arts and Social Sciences, Flinders University, South Australia.18 School of Earth, Ocean, and Environment, University of South Carolina, Columbia, South Carolina, United States of America.19 Planetary and Space Sciences, The Open University, Milton Keynes, United Kingdom.</affiliations>
    <journal>PloS one</journal>
    <writer>Moore CR;Tselmovich VA;LeCompte MA;West A;Culver SJ;Mallinson DJ;Baalousha M;Kennett JP;Napier WM;Bizimis M;Adedeji V;Sutton SR;Kletetschka G;Langworthy KA;Perez JP;Witwer T;Young MD;Alam M;Jeffreys J;Greenwood RC;Malley JA;</writer>
    <author1>Christopher R Moore,Vladimir A Tselmovich,Malcolm A LeCompte,Allen West,Stephen J Culver,David J Mallinson,Mohammed Baalousha,James P Kennett,William M Napier,Michael Bizimis,Victor Adedeji,Seth R Sutton,Gunther Kletetschka,Kurt A Langworthy,Jesus P Perez</author1>
    <author><![CDATA[Christopher R Moore&nbsp; 1&nbsp; 2,&nbsp;Vladimir A Tselmovich&nbsp; 3,&nbsp;Malcolm A LeCompte&nbsp; 4,&nbsp;Allen West&nbsp; 5,&nbsp;Stephen J Culver&nbsp; 6,&nbsp;David J Mallinson&nbsp; 6,&nbsp;Mohammed Baalousha&nbsp; 7,&nbsp;James P Kennett&nbsp; 8,&nbsp;William M Napier&nbsp; 9,&nbsp;Michael Bizimis&nbsp; 10,&nbsp;Victor Adedeji&nbsp; 11,&nbsp;Seth R Sutton&nbsp; 12,&nbsp;Gunther Kletetschka&nbsp; 13&nbsp; 14,&nbsp;Kurt A Langworthy&nbsp; 15,&nbsp;Jesus P Perez&nbsp; 16,&nbsp;Timothy Witwer&nbsp; 5,&nbsp;Marc D Young&nbsp; 17,&nbsp;Mahbub Alam&nbsp; 7,&nbsp;Jordan Jeffreys&nbsp; 18,&nbsp;Richard C Greenwood&nbsp; 19,&nbsp;James A Malley&nbsp; 19]]></author>
    <date>2025</date>
    <ftitle>记录在巴芬湾多个岩芯中的含有微球体和铂异常的1.28万年前彗星尘层</ftitle>
    <pmid>40768403</pmid>
    <keywordcn>彗星尘埃,微球体,铂异常</keywordcn>
  </doc>
  <doc index="7" percent="">
    <id>1055857</id>
    <classid>525</classid>
    <newstime>1741575001</newstime>
    <tbname>med9</tbname>
    <title>Microbial ecosystems and ecological driving forces in the deepest ocean sediments</title>
    <autocomplete>Microbial ecosystems and ecological driving forces in the deepest ocean sediments</autocomplete>
    <citation>2025 Mar 6;188(5):1363-1377.e9.</citation>
    <doi>10.1016/j.cell.2024.12.036</doi>
    <enabstracts>Systematic exploration of the hadal zone, Earth's deepest oceanic realm, has historically faced technical limitations. Here, we collected 1,648 sediment samples at 6-11 km in the Mariana Trench, Yap Trench, and Philippine Basin for the Mariana Trench Environment and Ecology Research (MEER) project. Metagenomic and 16S rRNA gene amplicon sequencing generated the 92-Tbp MEER dataset, comprising 7,564 species (89.4% unreported), indicating high taxonomic novelty. Unlike in reported environments, neutral drift played a minimal role, while homogeneous selection (HoS, 50.5%) and dispersal limitation (DL, 43.8%) emerged as dominant ecological drivers. HoS favored streamlined genomes with key functions for hadal adaptation, e.g., aromatic compound utilization (oligotrophic adaptation) and antioxidation (high-pressure adaptation). Conversely, DL promoted versatile metabolism with larger genomes. These findings indicated that environmental factors drive the high taxonomic novelty in the hadal zone, advancing our understanding of the ecological mechanisms governing microbial ecosystems in such an extreme oceanic environment.                                                                                                                  Keywords:                    16S rRNA gene amplicon; Mariana Trench; adaptation strategies; community assembly; ecological processes; hadal microbiome; hadal zone; metagenomic sequencing.                      Copyright © 2025 The Authors. Published by Elsevier Inc. All rights reserved.</enabstracts>
    <journal2>Cell</journal2>
    <issn>1097-4172</issn>
    <affiliations>1 State Key Laboratory of Microbial Metabolism, International Center for Deep Life Investigation (IC-DLI), School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China. Electronic address: zjxiao2018@sjtu.edu.cn.2 State Key Laboratory of Microbial Metabolism, International Center for Deep Life Investigation (IC-DLI), School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China. Electronic address: zwsh88@sjtu.edu.cn.3 BGI Research, Sanya 572025, China; BGI Research, Shenzhen 518083, China; Shenzhen Key Laboratory of Environmental Microbial Genomics and Application, BGI Research, Shenzhen 518083, China.4 State Key Laboratory of Microbial Metabolism, International Center for Deep Life Investigation (IC-DLI), School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China.5 China National GeneBank, BGI Research, Shenzhen 518083, China; Shenzhen Key Laboratory of Environmental Microbial Genomics and Application, BGI Research, Shenzhen 518083, China.6 BGI Research, Sanya 572025, China; BGI Research, Shenzhen 518083, China.7 Center for High Performance Computing, Shanghai Jiao Tong University, Shanghai, China.8 State Key Laboratory of Microbial Metabolism, International Center for Deep Life Investigation (IC-DLI), School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China; School of Oceanography, Shanghai Jiao Tong University, Shanghai, China; Shanghai Jiao Tong University Hainan Research Institute, Sanya 572025, China.9 State Key Laboratory of Microbial Metabolism, International Center for Deep Life Investigation (IC-DLI), School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China; Shanghai Jiao Tong University Hainan Research Institute, Sanya 572025, China.10 BGI Research, Qingdao 266555, China; Institute of Metagenomics, Qingdao-Europe Advance Institute for Life Sciences, BGI Research, Qingdao 266555, China; Laboratory of Genomics and Molecular Biomedicine, Department of Biology, University of Copenhagen, 2100 Copenhagen, Denmark.11 BGI Research, Shenzhen 518083, China; Shenzhen Key Laboratory of Environmental Microbial Genomics and Application, BGI Research, Shenzhen 518083, China.12 BGI Research, Qingdao 266555, China.13 China National GeneBank, BGI Research, Shenzhen 518083, China; Genomics Data Center of Guangdong Province, BGI Research, Shenzhen 518083, China.14 Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China.15 College of Marine Science and Technology, Hainan Tropical Ocean University, Sanya 572000, China.16 Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China; Institution of Deep-Sea Life Sciences, IDSSE-BGI, Hainan Deep-sea Technology Laboratory, Sanya, Hainan, China.17 School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.18 MGI Tech, Shenzhen 518083, China.19 China National GeneBank, BGI Research, Shenzhen 518083, China.20 BGI Research, Sanya 572025, China.21 BGI Research, Shenzhen 518083, China.22 China National GeneBank, BGI Research, Shenzhen 518083, China; BGI, Shenzhen 518083, China.23 BGI Research, Shenzhen 518083, China; Institute of Metagenomics, Qingdao-Europe Advance Institute for Life Sciences, BGI Research, Qingdao 266555, China; Laboratory of Genomics and Molecular Biomedicine, Department of Biology, University of Copenhagen, 2100 Copenhagen, Denmark.24 BGI, Shenzhen 518083, China.25 Institute of Environment and Ecology, Tsinghua Shenzhen International Graduate School, Tsinghua University, Shenzhen 518055, China.26 Institute for Environmental Genomics, University of Oklahoma, Norman, OK 73019, USA; School of Biological Sciences, University of Oklahoma, Norman, OK 73019, USA; School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK 73019, USA; School of Computer Sciences, University of Oklahoma, Norman, OK 73019, USA; Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.27 Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China; Institution of Deep-Sea Life Sciences, IDSSE-BGI, Hainan Deep-sea Technology Laboratory, Sanya, Hainan, China. Electronic address: wzhang@idsse.ac.cn.28 BGI Research, Sanya 572025, China; BGI Research, Shenzhen 518083, China; Laboratory of Genomics and Molecular Biomedicine, Department of Biology, University of Copenhagen, 2100 Copenhagen, Denmark; Shenzhen Key Laboratory of Environmental Microbial Genomics and Application, BGI Research, Shenzhen 518083, China. Electronic address: hanmo@genomics.cn.29 BGI Research, Shenzhen 518083, China; Guangdong Provincial Key Laboratory of Genome Read and Write, BGI Research, Shenzhen 518083, China. Electronic address: xuxun@genomics.cn.30 BGI Research, Qingdao 266555, China; MGI Tech, Shenzhen 518083, China; Shenzhen Key Laboratory of Marine Genomics, BGI Research, Shenzhen 518083, China; Institution of Deep-Sea Life Sciences, IDSSE-BGI, Hainan Deep-sea Technology Laboratory, Sanya, Hainan, China. Electronic address: liushanshan@mgi-tech.com.</affiliations>
    <journal>Cell</journal>
    <writer>Xiao X;Zhao W;Song Z;Qi Q;Wang B;Zhu J;Lin J;Wang J;Hu A;Huang S;Wang Y;Chen J;Fang C;Ji Q;Zhang N;Meng L;Wei X;Chen C;Cai S;Chen S;Ding K;Li D;Liu S;Song T;Tian L;Zhang H;Zhang Y;Xu S;Chen J;Chen H;Cen Q;Jiang F;Hu G;Tang C;Guo W;Wang X;Zhan L;Fan J;Wang</writer>
    <author1>Xiang Xiao,Weishu Zhao,Zewei Song,Qi Qi,Bo Wang,Jiahui Zhu,James Lin,Jing Wang,Aoran Hu,Shanshan Huang,Yinzhao Wang,Jianwei Chen,Chao Fang,Qianyue Ji,Nannan Zhang,Liang Meng,Xiaofeng Wei,Chuanxu Chen,Shanya Cai,Shun Chen,Kang Ding,Dong Li,Shuangquan Liu,T</author1>
    <author><![CDATA[Xiang Xiao&nbsp; 1,&nbsp;Weishu Zhao&nbsp; 2,&nbsp;Zewei Song&nbsp; 3,&nbsp;Qi Qi&nbsp; 4,&nbsp;Bo Wang&nbsp; 5,&nbsp;Jiahui Zhu&nbsp; 6,&nbsp;James Lin&nbsp; 7,&nbsp;Jing Wang&nbsp; 8,&nbsp;Aoran Hu&nbsp; 4,&nbsp;Shanshan Huang&nbsp; 9,&nbsp;Yinzhao Wang&nbsp; 4,&nbsp;Jianwei Chen&nbsp; 10,&nbsp;Chao Fang&nbsp; 11,&nbsp;Qianyue Ji&nbsp; 12,&nbsp;Nannan Zhang&nbsp; 12,&nbsp;Liang Meng&nbsp; 12,&nbsp;Xiaofeng Wei&nbsp; 13,&nbsp;Chuanxu Chen&nbsp; 14,&nbsp;Shanya Cai&nbsp; 14,&nbsp;Shun Chen&nbsp; 14,&nbsp;Kang Ding&nbsp; 14,&nbsp;Dong Li&nbsp; 14,&nbsp;Shuangquan Liu&nbsp; 14,&nbsp;Taoran Song&nbsp; 15,&nbsp;Liyang Tian&nbsp; 14,&nbsp;Haibin Zhang&nbsp; 16,&nbsp;Yu Zhang&nbsp; 17,&nbsp;Shiyu Xu&nbsp; 18,&nbsp;Jiayu Chen&nbsp; 19,&nbsp;Haixin Chen&nbsp; 20,&nbsp;Qian Cen&nbsp; 19,&nbsp;Fangfang Jiang&nbsp; 19,&nbsp;Guohai Hu&nbsp; 5,&nbsp;Chenguang Tang&nbsp; 18,&nbsp;Wu Guo&nbsp; 7,&nbsp;Xiaohan Wang&nbsp; 21,&nbsp;Liping Zhan&nbsp; 12,&nbsp;Jie Fan&nbsp; 12,&nbsp;Jun Wang&nbsp; 20,&nbsp;Changhao Zhou&nbsp; 12,&nbsp;Liuyang Li&nbsp; 4,&nbsp;Zhenbo Lv&nbsp; 4,&nbsp;Yaoxun Hu&nbsp; 4,&nbsp;Xiaonan Lin&nbsp; 20,&nbsp;Guoqiang Mai&nbsp; 19,&nbsp;Linlin Luo&nbsp; 19,&nbsp;Tao Yang&nbsp; 22,&nbsp;Weiwen Wang&nbsp; 22,&nbsp;Karsten Kristiansen&nbsp; 23,&nbsp;Liqun Chen&nbsp; 19,&nbsp;Huanming Yang&nbsp; 24,&nbsp;Ming Ni&nbsp; 18,&nbsp;Ying Gu&nbsp; 21,&nbsp;Feng Mu&nbsp; 18,&nbsp;Yunfeng Yang&nbsp; 25,&nbsp;Jizhong Zhou&nbsp; 26,&nbsp;Jian Wang&nbsp; 24,&nbsp;Wei-Jia Zhang&nbsp; 27,&nbsp;Mo Han&nbsp; 28,&nbsp;Xun Xu&nbsp; 29,&nbsp;Shanshan Liu&nbsp; 30]]></author>
    <date>2025</date>
    <pmid>40054447</pmid>
    <ftitle>最深海洋沉积物中的微生物生态系统及其生态驱动因素</ftitle>
    <keyboard>microbial ecosystems,ecological driving forces,ocean sediments</keyboard>
    <keywordcn>微生物生态系统,生态驱动因素,海洋沉积物</keywordcn>
  </doc>
  <doc index="8" percent="">
    <id>953479</id>
    <classid>521</classid>
    <newstime>1739778778</newstime>
    <tbname>med9</tbname>
    <title>Unveiling the deep-sea microplastic Odyssey: Characteristics, distribution, and ecological implications in Pacific Ocean sediments</title>
    <autocomplete>Unveiling the deep-sea microplastic Odyssey: Characteristics, distribution, and ecological implications in Pacific Ocean sediments</autocomplete>
    <citation>2025 Feb 12:489:137537.</citation>
    <doi>10.1016/j.jhazmat.2025.137537</doi>
    <enabstracts>Microplastics (MPs) in deep-sea environments are a growing concern due to their potential ecological risks and the deep sea's role in global biogeochemical cycles. This study investigated the characteristics and distribution of MPs in sediments from the Pacific Ocean at depths of 4900-7016 m across three regions: Western Pacific (WP), Central Pacific (CP), and Eastern Pacific (EP). MPs were detected at all sampling sites, with the highest abundance in WP (111.3 ± 75.1 items/kg dw) and the lowest in CP (49.4 ± 18.7 items/kg dw). Site S9 was recorded as the peak abundance (270.1 ± 107.4 items/kg dw) in WP. MPs were predominantly fibers (94.8 %) in black, gray, and blue hues, mainly composed of polyester and rayon. Statistical analysis showed significant regional variations, reflecting anthropogenic impacts and complex deposition mechanisms. Risk assessments indicated low to medium hazard levels (PLI</enabstracts>
    <journal2>J Hazard Mater</journal2>
    <issn>1873-3336</issn>
    <affiliations>1 Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China; National Engineering Research Center for Gas Hydrate Exploration and Development, Guangzhou 511458, China.2 College of Oceanography and Ecological Science, Shanghai Ocean University, Shanghai 201306, China; State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China. Electronic address: lsu@shou.edu.cn.3 Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China.4 State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China.5 Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China; National Engineering Research Center for Gas Hydrate Exploration and Development, Guangzhou 511458, China. Electronic address: dengyinan@126.com.</affiliations>
    <journal>Journal of hazardous materials</journal>
    <writer>Deng H;Fu Y;Su L;Chen D;Deng X;Hu B;Chen Y;Deng Y;</writer>
    <author1>Hua Deng,Yutao Fu,Lei Su,Daohua Chen,Xiguang Deng,Bo Hu,Yuye Chen,Yinan Deng</author1>
    <author><![CDATA[Hua Deng&nbsp; 1,&nbsp;Yutao Fu&nbsp; 1,&nbsp;Lei Su&nbsp; 2,&nbsp;Daohua Chen&nbsp; 1,&nbsp;Xiguang Deng&nbsp; 3,&nbsp;Bo Hu&nbsp; 4,&nbsp;Yuye Chen&nbsp; 4,&nbsp;Yinan Deng&nbsp; 5]]></author>
    <date>2025</date>
    <pmid>39952139</pmid>
    <ftitle>揭开深海微塑料奥德赛：太平洋洋底的特性、分布及生态影响</ftitle>
    <keyboard>deep-sea microplastic,characteristics,Pacific Ocean sediments,ecological implications</keyboard>
    <keywordcn>深海微塑料,特征,太平洋洋底沉积物,生态影响</keywordcn>
  </doc>
  <doc index="9" percent="">
    <id>783488</id>
    <classid>515</classid>
    <newstime>1736809628</newstime>
    <tbname>med9</tbname>
    <title>Niche Partitioning and Intraspecific Variation of Thaumarchaeota in Deep Ocean Sediments</title>
    <autocomplete>Niche Partitioning and Intraspecific Variation of Thaumarchaeota in Deep Ocean Sediments</autocomplete>
    <citation>2025 Jan;27(1):e70018.</citation>
    <doi>10.1111/1462-2920.70018</doi>
    <enabstracts><![CDATA[Deep-sea sediments contain a large number of Thaumarchaeota that are phylogenetically distinct from their pelagic counterparts. However, their ecology and evolutionary adaptations are not well understood. Metagenomic analyses were conducted on samples from various depths of a 750-cm sediment core collected from the Mariana Trench Challenger Deep. The abundance of Thaumarchaeota and archaeal amoA generally decreased with depth, except for an unexpected peak midway through the core. The thaumarchaeotal metagenome-assembled genomes were classified into diverse phylogenetic clusters associated with amoA-NP-γ, amoA-NP-θ, and amoA-NP-δ of ammonia-oxidising Thaumarchaeota and non-ammonia-oxidising lineages. The most abundant group was within amoA-NP-γ, which is usually found in coastal and shallow habitats, indicating potential niche expansion from marine shallow to hadal environments. This benthic group showed within-species genomic variations compared to the previously identified Hadal water group, suggesting microdiversification of hadal Thaumarchaeota along with niche separation between benthic and pelagic environments. Evolutionary adaptations associated with the benthic-to-pelagic transition included reduced genome size, loss of motility/cell adhesion, altered energy metabolism, and different mechanisms for substrate acquisition and regulation (e.g., ammonium). These findings offer new insights into the evolution of hadal Thaumarchaeota and demonstrate, for the first time, intraspecies-level genomic variation in Thaumarchaeota related to the benthic-versus-pelagic niche partitioning in the deep ocean.                                                                                                                  Keywords:                    Thaumarchaeota; evolutionary adaptation; microdiversity; niche partitioning.                      © 2025 John Wiley & Sons Ltd.]]></enabstracts>
    <journal2>Environ Microbiol</journal2>
    <issn>1462-2920</issn>
    <affiliations><![CDATA[1 Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, China.2 Laboratory for Marine Ecology and Environmental Science, Qingdao Marine Science and Technology Center, Qingdao, China.3 Key Laboratory of Evolution & Marine Biodiversity (Ministry of Education) and Institute of Evolution & Marine Biodiversity, Ocean University of China, Qingdao, China.4 Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, China.5 School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, Norfolk, UK.]]></affiliations>
    <journal>Environmental microbiology</journal>
    <writer>Liu R;He X;Ren G;Li DW;Zhao M;Lehtovirta-Morley L;Todd JD;Zhang XH;Liu J;</writer>
    <author1>Ronghua Liu,Xinxin He,Gaoyang Ren,Da-Wei Li,Meixun Zhao,Laura Lehtovirta-Morley,Jonathan D Todd,Xiao-Hua Zhang,Jiwen Liu</author1>
    <author><![CDATA[Ronghua Liu&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Xinxin He&nbsp; 1,&nbsp;Gaoyang Ren&nbsp; 1,&nbsp;Da-Wei Li&nbsp; 2&nbsp; 4,&nbsp;Meixun Zhao&nbsp; 2&nbsp; 4,&nbsp;Laura Lehtovirta-Morley&nbsp; 5,&nbsp;Jonathan D Todd&nbsp; 5,&nbsp;Xiao-Hua Zhang&nbsp; 1&nbsp; 2&nbsp; 3,&nbsp;Jiwen Liu&nbsp; 1&nbsp; 2&nbsp; 3]]></author>
    <date>2025</date>
    <year2>2025 Jan</year2>
    <pmid>39777846</pmid>
    <ftitle>深海沉积物中古菌的生态分化及种内差异性研究</ftitle>
    <keyboard>niche partitioning,intraspecific variation,thaumarchaeota</keyboard>
    <keywordcn>生态位分化,种内变异,透射型古菌</keywordcn>
  </doc>
  <doc index="10" percent="">
    <id>763516</id>
    <classid>515</classid>
    <newstime>1736278220</newstime>
    <tbname>med9</tbname>
    <title>Predicting Climate Mitigation Through Carbon Burial in Blue Carbon Ecosystems-Challenges and Pitfalls</title>
    <autocomplete>Predicting Climate Mitigation Through Carbon Burial in Blue Carbon Ecosystems-Challenges and Pitfalls</autocomplete>
    <citation>2025 Jan;31(1):e70022.</citation>
    <doi>10.1111/gcb.70022</doi>
    <enabstracts><![CDATA[The concept of "blue carbon" is, in this study, critically evaluated with respect to its definitions, measuring approaches, and time scales. Blue carbon deposited in ocean sediments can only counteract anthropogenic greenhouse gas (GHG) emissions if stored on a long-term basis. The focus here is on the coastal blue carbon ecosystems (BCEs), mangrove forests, saltmarshes, and seagrass meadows due to their high primary production and large carbon stocks. Blue carbon sequestration in BCEs is typically estimated using either: 1. sediment carbon inventories combined with accretion rates or 2. carbon mass balance between input to and output from the sediment. The inventory approach is compromised by a lack of accurate accretion estimates over extended time periods. Hence, short-term sedimentation assays cannot be reliably extrapolated to long timescales. The use of long-term tracers like 210Pb, on the other hand, is invalid in most BCEs due to sediment mobility by bioturbation and other physical disturbances. While the mass balance approach provides reasonable short-term (months) estimates, it often fails when extrapolated over longer time periods (> 100 years) due to climatic variations. Furthermore, many published budgets based on mass balance do not include all relevant carbon sources and sinks. Simulations of long-term decomposition of mangrove, saltmarsh (Spartina sp.), and eelgrass (Zostera sp.) litter using a 3-G exponential model indicate that current estimates of carbon sequestration based on the inventory and mass balance approaches are 3-18 times too high. Most published estimates of carbon sequestration in BCEs must therefore be considered overestimates. The climate mitigation potential of blue carbon in BCEs is also challenged by excess emissions of the GHG methane (CH4) and nitrous oxide (N2O) from biogenic structures in mangrove forests and saltmarsh sediments. Thus, in many cases, carbon sequestration into BCE sediments cannot keep pace with the simultaneous GHG emissions in CO2 equivalents.                                                                                                                  Keywords:                    blue carbon ecosystem; carbon sequestration; decomposition; greenhouse gas; mangrove; saltmarsh; seagrass.                      © 2025 John Wiley & Sons Ltd.]]></enabstracts>
    <journal2>Glob Chang Biol</journal2>
    <issn>1365-2486</issn>
    <affiliations>1 Department of Biology, University of Southern Denmark, Odense, Denmark.</affiliations>
    <journal>Global change biology</journal>
    <writer>Kristensen E;Flindt MR;Quintana CO;</writer>
    <author1>Erik Kristensen,Mogens R Flindt,Cintia O Quintana</author1>
    <author><![CDATA[Erik Kristensen&nbsp; 1,&nbsp;Mogens R Flindt&nbsp; 1,&nbsp;Cintia O Quintana&nbsp; 1]]></author>
    <date>2025</date>
    <year2>2025 Jan</year2>
    <pmid>39757865</pmid>
    <pubtype>Review</pubtype>
    <ftitle>预测通过蓝色碳汇生态系统中的碳封存来进行气候缓解-挑战与困境</ftitle>
    <keyboard>climate mitigation,carbon burial,blue carbon ecosystems</keyboard>
    <keywordcn>气候缓解,碳封存,蓝色碳生态系统</keywordcn>
  </doc>
</es:result>
