The Role of Cyanobacteria in the Formation of Dendrolites: An Example from the Miaolingian Dendrolites, North China

IF 0.7 4区 地球科学 Q4 PALEONTOLOGY Paleontological Journal Pub Date : 2024-06-20 DOI:10.1134/s0031030123600099
Chung-Il Ri, Sang-Ho Kim, Yi-Dan Zhu, Xuan-Wang, Won-Hak Jo
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Abstract

Dendrolites that are characterized by dendritic fabrics on the basis of mesostructure are dominated by isolated dendritic clusters of calcimicrobes and are distinct from the laminated stromatolite. Dendrolites in the top part of the Miaolingian Zhangxia Formation at the Dongping section in Dongping County of Shandong province make up huge microbial reef with the thickness of 60 m that are developed in the sea-level falling period, which represent a spectacularly sedimentological phenomenon. Dendrolites are made from calcimicrobes belong to fossils of the Epiphyton group and Hedstroemia group. Microscopically, the bifurcating filamentous tip show bent or broken phenomenon, and the edges of thallus received partially negligible encrustation. This can reflect biological response to extreme environments. In addition, the morphological features of shrub thalli growing upwards and the branched morphology that shows the basic dendritic growth structure in particular, truthfully show the basic characteristics of dendrolites. This phenomenon can reflect the biological properties of microorganisms trying to maintain their own growth structures. The micritic crusts may reflect that the study area dendrolites were formed by sophisticated calcification of EPS that form microbial biofilms in microbial mats dominated by cyanobacteria. Therefore, microbial reef predominated by dendrolites in the top part of the Miaolingian Zhangxia Formation at the Dongping section are a typical example of demonstrating the fundamental characteristics of dendrolites different from clotted thrombolite, and further, provide some clues for the study of the biological attributes and responses between microorganisms and environments.

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蓝藻在树枝石形成过程中的作用:以华北庙岭石斛岩为例
摘要 在中生构造基础上以树枝状构造为特征的枝状岩以孤立的树枝状钙钛矿团为主,有别于层状叠层岩。山东省东平县东平断面庙岭张夏地层上部的树枝状岩构成了巨大的微生物礁,厚度达 60 米,发育于海平面下降期,是一种壮观的沉积现象。树枝状岩由钙钛矿化石组成,属于表生类和海带类化石。显微镜下,分叉的丝状顶端呈现弯曲或断裂现象,菌体边缘有部分可忽略不计的包壳。这可能反映了生物对极端环境的反应。此外,灌木铊向上生长的形态特征,特别是呈现树枝状基本生长结构的分枝形态,如实反映了树枝状植物的基本特征。这种现象可以反映微生物试图维持自身生长结构的生物特性。微晶结壳可能反映了研究区域的树枝状岩是由蓝藻为主的微生物垫中形成微生物生物膜的 EPS 经过复杂的钙化形成的。因此,东平剖面庙岭张夏地层上部以树枝状岩为主的微生物礁是展示树枝状岩不同于凝块血栓岩基本特征的典型实例,并为研究微生物与环境之间的生物属性和反应提供了一些线索。
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来源期刊
Paleontological Journal
Paleontological Journal 地学-古生物学
CiteScore
1.20
自引率
33.30%
发文量
70
审稿时长
6-12 weeks
期刊介绍: Paleontological Journal (Paleontologicheskii zhurnal) is the principal Russian periodical in paleontology. The journal publishes original work on the anatomy, morphology, and taxonomy of fossil organisms, as well as their distribution, ecology, and origin. It also publishes studies on the evolution of organisms, ecosystems, and the biosphere and provides invaluable information on global biostratigraphy with an emphasis on Eastern Europe and Asia.
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