New Benthic Fossils from the Late Ediacaran Strata of Southwestern China

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Junping LIU, Ming LI, Feng TANG, Jiangtai ZHAO, Sicun SONG, Ying ZHOU, Xiaohan SONG, Liudong REN
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引用次数: 0

Abstract

The Jiangchuan Biota from the Jiucheng Member (Mb.) of the Dengying Formation (Fm.), discovered in Jiangchuan, eastern Yunnan, China, is marked by copious macrofossils at the apex of the Ediacaran strata. This fauna features benthic algae with varied holdfasts and other fossils of indeterminate taxonomic affinity and is compositionally unique compared to the Shibantan and Gaojiashan biotas of the Dengying Fm. and the Miaohe and Wenghui biotas of the Doushantuo Fm., elsewhere in China. One novel benthic saccular macroalgal fossil, named here Houjiashania yuxiensis gen. and sp. nov., from the Jiangchuan Biota is based on fossils that are sausage-shaped, elongate, tubular, ranging from 0.3 to 4 cm in length, and up to 0.8 cm in diameter. One terminus is blunt and rounded to an obtuse angle, the other is bent with a spread-out surface resembling a holdfast, suggesting a three-dimensional thallus. Thin, stipe-shaped outgrowths, likely vestiges of sessile saccular life forms, are prevalent in macroalgal fossils of analogous size and shape, as well as present brown algae Scytosiphonaceae, such as Colpomenia and Dactylosiphon. The new findings augment the diversity of benthic algae, such as those known from the Early Neoproterozoic Longfengshan Biota in North China. The benthic algal macrofossils in the Jiucheng Mb. add to knowledge of Late Ediacaran metaphyte diversification and offer more clues about the evolutionary positioning of primitive macroalgae. The co-occurrence of numerous planktonic and benthic multicellular algae and planktonic microbes might have facilitated ecologically the more extensive later Cambrian explosion evidenced by the Chengjiang Biota in Yunnan.

Abstract Image

中国西南埃迪卡拉晚期地层中的新底栖化石
在中国云南东部江川发现的江川生物群位于埃迪卡拉纪地层的顶端,其特征是来自登瀛层九成组的大量大型化石。这批化石的特点是底栖藻类与各种固着物,以及分类亲缘关系不确定的大型化石。与登瀛层的石板滩生物群和高家山生物群以及斗山坨层的庙河生物群和汶水生物群相比,它在成分上具有独特性。本研究介绍了江川生物群中一种新的底栖囊状大型藻类化石。这些化石呈香肠状,拉长,管状,长 0.3 至 4 厘米,直径达 0.8 厘米。其中一个末端钝圆成钝角,另一个末端弯曲,表面平展,像一个固着器,表明这是一个三维的菌丝体。在具有类似大小和形状的大型藻类化石中,普遍存在细长的柄状突起,很可能是无柄囊状生命形式的遗迹。这一发现丰富了华北龙凤山生物群已知的新近纪早期底栖藻类的多样性。云南东部九成组底栖大型藻类化石可能会增加晚埃迪卡拉元古代藻类多样化的证据,并为原始大型藻类的演化定位提供更多线索。大量浮游和底栖多细胞藻类与浮游微生物的同时出现,可能在生态学上促进了澄江生物群所证明的更广泛的寒武纪大爆发。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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