Results 131 to 140 of about 671 (189)
Labechia aldonensis sp.nov.; an Ordovician stromatoporoid from Scotland
, 1977 B. D. Webby
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Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events [PDF]
Philos Trans R Soc Lond B Biol Sci, 1998 europepmc +1 more source
Impact structures in Africa: A review.
J Afr Earth Sci, 2014 Reimold WU, Koeberl C.
europepmc +1 more source
Understanding Palaeozoic stromatoporoid growth [PDF]
Earth-Science Reviews, 2018 Stromatoporoids were abundant components of reefs, reef complexes and associated facies for ca. 100 million years between Middle Ordovician and end-Devonian time. A lot of environmental information stored in their skeletons may be used to develop: a) understanding of stromatoporoid growth controls; and b) interpretations of sedimentary environments in ...
Emilia Jarochowska +2 more
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Earliest known rugosan-stromatoporoid symbiosis from the Llandovery of Estonia (Baltica)
Palaeogeography, Palaeoclimatology, Palaeoecology, 2015 A stromatoporoid, Petridiostroma simplex, from the Llandovery of Estonia was infested by numerous rugosan endobiotic symbionts of the species Petrozium losseni (Dybowski, 1874).
Olev Vinn, Mark A. Wilson, Ursula Toom
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Stromatoporoids and extinctions
2023Stromatoporoids are common shallow marine hypercalcified sponges in two major episodes with distinctive skeletal architectures: 1) Palaeozoic: Early to Middle Ordovician, to Late Devonian; and 2) Mesozoic: Late Triassic to Cretaceous and rare Cenozoic, but not confirmed in Permian and earlier Triassic strata. Stromatoporoids appeared in Early to Middle
Stephen Kershaw, Juwan Jeon
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