On Thu, 25 Mar 2021 08:57:41 -0700 (PDT), erik simpson
>Ediacaran (635–542?million years ago) fossils have been regarded as early animal ancestors of the Cambrian evolutionary explosion of marine invertebrate phyla1, as giant marine protists2 and as lichenized fungi3. Recent documentation of palaeosols in the Ediacara Member of the Rawnsley Quartzite of South Australia4 confirms past interpretations of lagoonal–aeolian deposition based on synsedimentary ferruginization and loessic texture5,6. Further evidence for palaeosols comes from non-marine facies, dilation cracks, soil nodules, sand crystals, stable isotopic data and mass balance geochemistry4. Here I show that the uppermost surfaces of the palaeosols have a variety of fossils in growth position, including Charniodiscus, Dickinsonia, Hallidaya, Parvancorina, Phyllozoon, Praecambridium, Rugoconites, Tribrachidium and ‘old-elephant skin’ (ichnogenus Rivularites7). These fossils were preserved as ferruginous impressions, like plant fossils8, and biological soil crusts9,10 of
>Phanerozoic eon sandy palaeosols. Sand crystals after gypsum11 and nodules of carbonate12 are shallow within the palaeosols4, even after correcting for burial compaction13. Periglacial involutions and modest geochemical differentiation of the palaeosols are evidence of a dry, cold temperate Ediacaran palaeoclimate in South Australia4. This new interpretation of some Ediacaran fossils as large sessile organisms of cool, dry soils, is compatible with observations that Ediacaran fossils were similar in appearance and preservation to lichens and other microbial colonies of biological soil crusts3, rather than marine animals1, or protists2.
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https://www.nature.com/articles/nature11777
You and Harshman make a good team. I acknowledge I didn't recognize
the implication of your statements wrt "fossil soils" being
necessarily terrestrial. But since this thread has finally arrived at
the heart of the matter:
<
https://astrobiology.nasa.gov/nai/media/medialibrary/2015/07/tarhanetal2015_pcubed_ediacaranissue.pdf>
<
https://tinyurl.com/ydhn6ed4>
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A careful assessment of paleoenvironmental parameters is essential to
the reconstruction of the depositional and early diagenetic history of
the Ediacara Biota and thus the physical, chemical and biological
factors that shaped the development and the fossilization of these
earliest examples of complex life. We find no compelling evidence for
a terrestrial setting for the Ediacara Member and strong support
for a shallow marine depositional environment.
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IIUC the consensus is the evidence Retallack describes in your cite is
consistent with shallow marine pools which repeatedly dried up and
refilled.
Also, my understanding is these taxa disappeared from the fossil
record during the Cambrian, even as these types of paleosols continued
through time. This suggests to me these taxa were aquatic organisms
which went extinct as newer lifeforms evolved. This explanation
doesn't work if these were terrestrial lichens, which had no known
competition during the Ediacaran and the Cambrian.
Also, I don't know if these taxa are found only in this particular
strata, or how many different types of Ediacaran strata exist. If
these taxa are found in other Ediacaran strata, this would be evidence
against their terrestrial origin.