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pro vyhledávání: '"Liu AG"'
Macrofossils of the late Ediacaran Period (c. 579–539 Ma) document diverse, complex multicellular eukaryotes, including early animals, prior to the Cambrian radiation of metazoan phyla. To investigate the relationships between environmental perturb
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1821505241b317e241020104a175d5e
https://www.repository.cam.ac.uk/handle/1810/324597
https://www.repository.cam.ac.uk/handle/1810/324597
The landscapes and seascapes of Earth’s surface provide the theatre for life, but to what extent did the actors build the stage? The role of life in the long-term shaping of the planetary surface needs to be understood to ascertain whether Earth is
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::63c8655b29123d2f535a7f23a4068272
Publikováno v:
Liu, A G, McMahon, S, Matthews, J J, Still, J W & Brasier, A T 2019, ' Petrological evidence in support of the death mask model for Ediacaran soft-bodied preservation in South Australia ', Geology . https://doi.org/10.1130/G45918.1
Microbially mediated early diagenetic pyrite formation in the immediate vicinity of organic material has been the favoured mechanism by which to explain widespread preservation of soft-bodied organisms in late Ediacaran sedimentary successions, but a
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d731b4525786c7476a08120ac513bc05
https://www.repository.cam.ac.uk/handle/1810/291011
https://www.repository.cam.ac.uk/handle/1810/291011
We thank Noffke (2017) for her comment and for providing an opportunity to clarify our classification of “sedimentary surface textures”. We accord great credit to Dr. Noffke and other dedicated researchers whose detailed work has brought microbia
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https://explore.openaire.eu/search/publication?articleId=od_______109::d7c22a7b494465e509ae8cd19331db1f
https://www.repository.cam.ac.uk/handle/1810/273165
https://www.repository.cam.ac.uk/handle/1810/273165
Autor:
Parry, L, Boggiani, PC, Condon, D, Garwood, R, Leme, J, McIlrory, D, Brasier, MD, Campanha, GAC, Pacheco, AF, Diniz, CQC, Liu, AG
The evolutionary events during the Ediacaran–Cambrian transition (~541 Ma) are unparalleled in Earth history. The fossil record suggests that most extant animal phyla appeared in a geologically brief interval, with the oldest unequivocal bilaterian
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::875f79504da617a2a55f7b82ac2abcaf
https://www.repository.cam.ac.uk/handle/1810/267109
https://www.repository.cam.ac.uk/handle/1810/267109
Fossil assemblages from Newfoundland’s Avalon Peninsula preserve diverse examples of the enigmatic Ediacaran macrobiota, offering some of the earliest evidence for large and complex multicellular life. These fossils are exposed on extensive coastal
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aca405a29f6da3eccc96cc2fc3c09c7b
https://www.repository.cam.ac.uk/handle/1810/262112
https://www.repository.cam.ac.uk/handle/1810/262112
Ediacaran structures known as 'pizza discs' or Ivesheadia have long been considered enigmatic. They are amongst the oldest known members of the Ediacara biota, apparently restricted to the Avalonian successions of Newfoundland and the UK, c. 579-560M
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::497b0e1f319537362f7eaabdc57a0db0
https://doi.org/10.1111/j.1475-4983.2010.01024.x
https://doi.org/10.1111/j.1475-4983.2010.01024.x
Ongoing discoveries of new rangeomorph fossils from the Ediacaran of Avalonia allow us to put forward a unified and approachable scheme for the description and phylogenetic analysis of frondose genera and their species. This scheme focuses upon the b
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7a4606b622b69550f666ca2c40b8f3fa
https://ora.ox.ac.uk/objects/uuid:e28c4240-383e-4a90-b8f3-23c0ab1b4e73
https://ora.ox.ac.uk/objects/uuid:e28c4240-383e-4a90-b8f3-23c0ab1b4e73