Huainan biota

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Location of Huainan City, Anhui Province, China Location of Huainan Prefecture within Anhui (China).png
Location of Huainan City, Anhui Province, China

The Huainan biota is a collection of macroscopic organisms discovered in the early 1980s in the Precambrian deposits of China (Huainan City, Anhui Province), that represent a transitional period in evolution. [1]

Contents

Discovery and age

Huainan biota organisms were discovered by Wang Guixiang and Sun Weiguo in the 1980s in Precambrian rock formations near Huainan City. [1] The organisms date back to 840-740 million years ago (Ma). [2] This falls into to the Tonian period, which marks a transitional phase in Earth's history where life began evolving from tiny micro-organisms to larger organisms. [3]

Geologic setting

In the Huainan area, the Neoproterozoic rock layers are classified in three main groups; the Huainan Group, Feishui Group, and the Fengtai Formation. [3] They each represent a different sedimentary cycle. [3] The Huainan group is made up of siliciclastic rocks like sandstone and shale. [3] The Feishui group consists of carbonate rocks, like limestone and dolomite, and includes fossil-bearing formations, such as the Jiuliqiao Formation, where the Huainan Biota was found. [3] The Fengtai Formation is composed of glacial deposits of diamictites. [3]

A Tonian-age organism visually similar to Huainan biota fossils: Tawuia dalensis from the Shiwangzhuang Formation. Tawuia dalensis, Shiwangzhuang Formation, Tumen Group (North China).jpg
A Tonian-age organism visually similar to Huainan biota fossils: Tawuia dalensis from the Shiwangzhuang Formation.

Fossil description

Two types of Huainan biota were found in the Jiuliqiao Formation, a geological rock unit ranging from 26 to 119 meters thick, dating to the Ediacaran Period. [4] Their difference being in their fossil shapes. The first type of biota consists of a worm-like, tubular structure. [4] The second type of biota consists of solitary discs with a central opening. [4] Both fossil types vary between 0.5-2 mm in size. [4]

Similar biota

A similar biota, about 1 billion years old, was found by M. B. Gnilovskaya in Russia on the Timan Ridge. [5] It is only known that its constituent organisms ( Protoarenicola , Pararenicola , Sinosabellidites ) reached several centimeters in size (which is significantly inferior to the Ediacaran ones) and, apparently, had the shape of segmented tubes, often goblet-shaped, with extensions at the end. [5] Huainan biota do not contain jellyfish-like "discs" (as seen in the Ediacaran biota), nor any forms close to sponges.

See also

References

  1. 1 2 Li, Guangjin; Chen, Lei; Pang, Ke; Tang, Qing; Wu, Chengxi; Yuan, Xunlai; Zhou, Chuanming; Xiao, Shuhai (2023-04-12). "Tonian carbonaceous compressions indicate that Horodyskia is one of the oldest multicellular and coenocytic macro-organisms". Communications Biology. 6 (1): 399. doi:10.1038/s42003-023-04740-2. ISSN   2399-3642. PMC   10097871 . PMID   37046079.
  2. Tang, Qing; Pang, Ke; Xiao, Shuhai; Yuan, Xunlai; Ou, Zhiji; Wan, Bin (2013-10-01). "Organic-walled microfossils from the early Neoproterozoic Liulaobei Formation in the Huainan region of North China and their biostratigraphic significance" . Precambrian Research. 236: 157–181. doi:10.1016/j.precamres.2013.07.019. ISSN   0301-9268.
  3. 1 2 3 4 5 6 Qin, Shujian; Dong, Lin; Liu, Xuan; Tang, Feng; Liu, Hui (2023-08-01). "Macroscopic carbonaceous compression fossils from the Tonian Liulaobei Formation in the Huainan region of North China" . Precambrian Research. 393: 107076. doi:10.1016/j.precamres.2023.107076. ISSN   0301-9268.
  4. 1 2 3 4 Li, Guangjin; Pang, Ke; Tang, Qing; Chen, Lei; Wu, Chengxi; Huang, Rui; Wan, Bin; Yuan, Xunlai; Zhou, Chuanming (2023-10-15). "Tonian discoidal fossils from North China: Relating discs to worm-like annulated tubes and their paleoecological and evolutionary implications" . Palaeogeography, Palaeoclimatology, Palaeoecology. 628: 111780. doi:10.1016/j.palaeo.2023.111780. ISSN   0031-0182.
  5. 1 2 Fedonkin, Mikhail A. (2003). "The origin of the Metazoa in the light of the Proterozoic fossil record". Paleontological Research. 7 (1): 9–41. Bibcode:2003PalRe...7....9F. doi:10.2517/prpsj.7.9.

Further literature