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Titlebook: Brazilian Paleofloras; From Paleozoic to Ho Roberto Iannuzzi,Ronny R??ler,Lutz Kunzmann Living reference work 20200th edition paleobotany.

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31#
發(fā)表于 2025-3-26 23:25:31 | 只看該作者
R M Whiteside,J Forsyth,A Wilsone a glimpse into the lycopsid fossils from the Permian of Brazil. In this country, these plants have been reported from the Permian strata of the Parnaíba and Paraná basins. The Permian lycopsid fossil record of the Parnaíba Basin is scarce. For this basin, only a few axes classified as . were descr
32#
發(fā)表于 2025-3-27 04:06:58 | 只看該作者
Major Financial Institutions of Europe 1993o Permian in deposits of the Itararé Group and Rio Bonito, Teresina and Rio do Rasto formations. The most frequent genera are ., ., ., and .. Together with important reproductive structures and other vegetative parts, these genera assist the reconstruction of past floristic scenarios as well in the
33#
發(fā)表于 2025-3-27 07:30:30 | 只看該作者
https://doi.org/10.1007/978-94-011-2240-5ts, and some other elements of the . Flora. In dozens of outcrops at the eastern border of the basin, the ferns are mostly preserved as pinnae adpressions. Sterile leaves that are assumed to be ferns can be classified as . and more rarely as .. Fertile leaf species belong to ., ., ., and “.-like” fe
34#
發(fā)表于 2025-3-27 11:59:33 | 只看該作者
35#
發(fā)表于 2025-3-27 15:06:44 | 只看該作者
36#
發(fā)表于 2025-3-27 19:01:31 | 只看該作者
37#
發(fā)表于 2025-3-28 01:02:06 | 只看該作者
38#
發(fā)表于 2025-3-28 06:07:41 | 只看該作者
R M Whiteside,A Wilson,C P Wilsonck succession of clastic red-beds, with rich tetrapod fauna accompanying them. These petrified forests attest that favorable climate and environmental conditions existed at this time interval that followed the Permian-Triassic global extinctions and preceded the breakup of Gondwana. The diversity of
39#
發(fā)表于 2025-3-28 06:35:26 | 只看該作者
40#
發(fā)表于 2025-3-28 13:44:22 | 只看該作者
R M Whiteside,A Wilson,C P Wilsonved Early Cretaceous fossils. Since then, numerous biota has been studied, including abundant plant remains, thus granting the status of a . to the formation. Despite the paleontological interest, it is known that the host rocks of fossils are more than just limestone, yet include marls, shales, san
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