第 6 章科拉半岛早新生代磷酸盐岩科拉半岛早新生代磷酸盐岩

IF 0.7 4区地球科学 Q4 PALEONTOLOGY

Paleontological Journal Pub Date : 2024-03-21 DOI:10.1134/s0031030124600069

M. M. Astafieva

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引用次数: 0

摘要

摘要年龄为 2.04 Ga 的佩钦嘎盆地磷酸盐岩是由微生物产生的。佩成雅绿岩带的磷酸盐岩以大量圆形、轻微变形的碎片形式被发现（图 1）。最早的早新生代（佩成阿）磷酸盐岩显示了蓝藻垫的所有特征--蓝藻垫是一种由糖萼结合成物理结构的原核底栖生物群落。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Chapter 6. Early Proterozoic Phosphorites of the Kola Peninsula

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Chapter 6. Early Proterozoic Phosphorites of the Kola Peninsula

Abstract

Phosphorites from the Pechenga Basin, with an age of 2.04 Ga, were produced by microorganisms. Phosphorites of the Pechenga Greenstone Belt were found in the form of numerous rounded, slightly deformed fragments (Fig. 1). The earliest Early Proterozoic (Pechenga) phosphorites show all the characteristics of a cyanobacterial mat—a prokaryotic benthic community united in a physical structure by the glycocalyx.

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来源期刊

Paleontological Journal 地学-古生物学

CiteScore

1.20

自引率

33.30%

发文量

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.

第 6 章 科拉半岛早新生代磷酸盐岩科拉半岛早新生代磷酸盐岩

摘要

Abstract

第 6 章科拉半岛早新生代磷酸盐岩科拉半岛早新生代磷酸盐岩