Climate Change Data Portal
DOI | 10.1111/gbi.12338 |
Holocene paleodepositional changes reflected in the sedimentary microbiome of the Black Sea | |
More K.D.; Giosan L.; Grice K.; Coolen M.J.L. | |
发表日期 | 2019 |
ISSN | 14724677 |
起始页码 | 436 |
结束页码 | 448 |
卷号 | 17期号:4 |
英文摘要 | Subsurface microbial communities are generally thought to be structured through in situ environmental conditions such as the availability of electron acceptors and donors and porosity, but recent studies suggest that the vertical distribution of a subset of subseafloor microbial taxa, which were present at the time of deposition, were selected by the paleodepositional environment. However, additional highly resolved temporal records of subsurface microbiomes and paired paleoenvironmental reconstructions are needed to justify this claim. Here, we performed a highly resolved shotgun metagenomics survey to study the taxonomic and functional diversity of the subsurface microbiome in Holocene sediments underlying the permanently stratified and anoxic Black Sea. Obligate aerobic bacteria made the largest contribution to the observed shifts in microbial communities associated with known Holocene climate stages and transitions. This suggests that the aerobic fraction of the subseafloor microbiome was seeded from the water column and did not undergo post-depositional selection. In contrast, obligate and facultative anaerobic bacteria showed the most significant response to the establishment of modern-day environmental conditions 5.2 ka ago that led to a major shift in planktonic communities and in the type of sequestered organic matter available for microbial degradation. No significant shift in the subseafloor microbiome was observed as a result of environmental changes that occurred shortly after the marine reconnection, 9 ka ago. This supports the general view that the marine reconnection was a gradual process. We conclude that a high-resolution analysis of downcore changes in the subseafloor microbiome can provide detailed insights into paleoenvironmental conditions and biogeochemical processes that occurred at the time of deposition. © 2019 John Wiley & Sons Ltd |
关键词 | anoxic conditionsbacteriumclimate variationHolocenein situ measurementmicrobial communityreconstructiontaxonomyvertical distributionwater columnBlack Seabacterial phenomena and functionsbacteriumBlack SeaBulgariaclassificationfossilgeneticsmetagenomemicrobiologymicroflorasedimentBacteriaBacterial Physiological PhenomenaBlack SeaBulgariaFossilsGeologic SedimentsMetagenomeMicrobiota |
语种 | 英语 |
来源机构 | Geobiology |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/133227 |
推荐引用方式 GB/T 7714 | More K.D.,Giosan L.,Grice K.,et al. Holocene paleodepositional changes reflected in the sedimentary microbiome of the Black Sea[J]. Geobiology,2019,17(4). |
APA | More K.D.,Giosan L.,Grice K.,&Coolen M.J.L..(2019).Holocene paleodepositional changes reflected in the sedimentary microbiome of the Black Sea.,17(4). |
MLA | More K.D.,et al."Holocene paleodepositional changes reflected in the sedimentary microbiome of the Black Sea".17.4(2019). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。