Development of aragonite crystals in the Neoproterozoic Nikol’skoe formation of the Ura uplift (East Siberia)


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

It is established that organogenic limestones of the Neoproterozoic (Upper Riphean) Nikol’skoe Formation contain aragonite crystals surrounding filamentous calcified algae, which take part in the formation of stromatolites. They indicate the possibility of the development of fine-fibrous, acicular, and prismatic aragonite crystals in the calcareous mud during the calcification of red algal thalluses (for example, genus Chaptchaica Kolosov) enveloped by a common thick gelatinous (during the organism life) sheath. The group of red algae, which concentrate lime in the form of aragonite crusts appeared not later than the Neoproterozoic (Late Riphean). A high-quality image of the cell nucleus was obtained for the first time from the Neoproterozoic red algae Chaptchaica viva Kolosov, 1975.

作者简介

P. Kolosov

Institute of the Geology of Diamond and Noble Metals, Siberian Branch

编辑信件的主要联系方式.
Email: p_kolosov@diamond.ysn.ru
俄罗斯联邦, Yakutsk, 677891

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Inc., 2017