Climate Change Data Portal
DOI | 10.1016/j.palaeo.2018.06.030 |
Small microbialites from the basal Triassic mudstone (Tieshikou; Jiangxi; South China): Geobiologic features; biogenicity; and paleoenvironmental implications | |
Yang H.; Chen Z.-Q.; Kershaw S.; Liao W.; Lü E.; Huang Y. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 221 |
结束页码 | 235 |
卷号 | 519 |
英文摘要 | We report small microbialites from the calcareous mudstone slightly above the Permian–Triassic boundary (PTB) in the Tieshikou section, southern Jiangxi Province, South China. The newly found microbialite is a bowl-like structure, which contrasts with the surrounding calcareous mudstone. The small microbialite is composed of columnar forms and fan-shaped structures. Mini-columnar structures resemble mini stromatolites. In plane view, most branches are patchy or strip-shaped, with clotted structures, resembling that of a thrombolite. Fan-shaped cement precipitates are comprised of multiple crystal fans that have a radiating texture and that show distinct growth laminae. The radiating fabrics are represented by rod-shaped filaments under SEM, which are interpreted as calcified trichomes/filaments. Prominent micropores occur within the rods, and they may be the plane views of multiple sheaths of the false branching zone of trichomes. Thus, both the columnar forms and radiating fans are probably microbial in origin. Moreover, three types of nano-sized structures: intraparticle micropores, fibrous biofilms, and filamentous sheaths are also pronounced in both the columnar structures and cement fans of the Tieshikou microbialite, all suggestive of biogenicity. These well-preserved fibrous biofilms probably represent calcified extracellular polymeric substances (EPS), and linear sheaths are interpreted as the traces of bacterial activities during the precipitation of dolomite crystals. The Tieshikou microbialite therefore shares similar biogenetic mechanisms with other PTB microbialites. The combination of the absence of pyrite framboids, slightly negative carbon isotope values, and an association with abundant ammonoids, bivalves, and gastropods indicates oxic conditions during the growth of the Tieshikou microbialite. Moreover, the nodular preservational state resembles widely distributed nodular mudstones or muddy limestones of the Lower Triassic successions worldwide. This implies that nodular mudstone or argillaceous limestones may also have been deposited in microbe-rich environments, in which terrigenous supply was abundant. © 2018 Elsevier B.V. |
英文关键词 | Clotted structure; Early Triassic; Limestone nodule; Mass extinction; Microbial bloom |
语种 | 英语 |
scopus关键词 | exopolymer; growth; invertebrate; limestone; mass extinction; microbialite; mudstone; paleoenvironment; precipitation (chemistry); stromatolite; Triassic; China; Ammonoidea; Bacteria (microorganisms); Bivalvia; Gastropoda |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151042 |
作者单位 | State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan, 430074, China; Department of Life Sciences, Brunel University, Kingston Lane, Uxbridge, UB8 3PH, United Kingdom |
推荐引用方式 GB/T 7714 | Yang H.,Chen Z.-Q.,Kershaw S.,et al. Small microbialites from the basal Triassic mudstone (Tieshikou; Jiangxi; South China): Geobiologic features; biogenicity; and paleoenvironmental implications[J],2019,519. |
APA | Yang H.,Chen Z.-Q.,Kershaw S.,Liao W.,Lü E.,&Huang Y..(2019).Small microbialites from the basal Triassic mudstone (Tieshikou; Jiangxi; South China): Geobiologic features; biogenicity; and paleoenvironmental implications.Palaeogeography, Palaeoclimatology, Palaeoecology,519. |
MLA | Yang H.,et al."Small microbialites from the basal Triassic mudstone (Tieshikou; Jiangxi; South China): Geobiologic features; biogenicity; and paleoenvironmental implications".Palaeogeography, Palaeoclimatology, Palaeoecology 519(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。