Buzzard3
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- Jan 31, 2022
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"According to Gaines et al. (2012),We also don't find a lot of pre-Cambrian life because the vast majority of pre-Cambrian life was softer than the harder organisms that came during and after the Cambrian Explosion, meaning they wouldn't fossilize well. Fossils form under specific circumstances. Those circumstances aren't met, the bones just go.
“Burgess Shale−type biotas occur globally in the Cambrian record and offer unparalleled insight into the Cambrian explosion, the initial Phanerozoic radiation of the Metazoa. Deposits bearing exceptionally preserved soft-bodied fossils are unusually common in Cambrian strata; more than 40 are now known.”
Thus, we definitely should expect to find the postulated ancestors of the Cambrian animal phyla in Burgess Shale-type localities of the preceding Ediacaran era. The artifact hypothesis suggested that there are no such localities. However, in the past years several fossiliferous Burgess Shale-type (BST) biota from the Ediacaran have been discovered:
Pusa Shale of Spain (Brasier et al. 1979, Jensen & Palacios 2016)
Chopoghlu Shale / Soltanieh Formation of northern Iran (Ford & Breed 1972)
Khatyspyt Formation of Siberia (Grazhdankin et al. 2008)
Miaohe biota of southern China (Xiao et al. 2002, Tang et al. 2008, Ye et al. 2017)
Lantian biota of southern China (Yuan et al. 2011, 2013)
Jinxian biota of northern China (Luo et al. 2016)
Zuun-Arts biota of western Mongolia (Dornbos et al. 2016, Hassell et al. 2017)
Guess What?
None of these Ediacaran biotas yielded any uncontroversial fossil record of animals! Especially important are the vast deposits of the Miaohe and Lantian biotas in China and the Zuun-arts biota in Mongolia, which both lack any bilaterian animals and only yielded fossil algae and problematic organisms ...
Even the most recent study by Daley et al. (2018), which very unsuccessfully (Bechly 2018a) tried to downplay the abruptness of the Cambrian explosion, acknowledged that these new localities have proven that fossil animals are not just unknown from the Ediacaran because of preservation issues but because they definitely did not yet exist. Daley et al. discussed all the above-mentioned Burgess Shale-type localities from the Ediacaran and concluded that the “modes of fossil preservation are comparable in the Cambrian and Precambrian.”
In their abstract they affirmed that: “BSTs from the latest Ediacaran Period (e.g., Miaohe biota, 550 Ma) are abundantly fossiliferous with algae but completely lack animals, which are also missing from other Ediacaran windows, such as phosphate deposits (e.g., Doushantuo, 560 Ma)”" ...
continued in next post ...
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