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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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41#
發(fā)表于 2025-3-28 15:13:07 | 只看該作者
42#
發(fā)表于 2025-3-28 19:01:19 | 只看該作者
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43#
發(fā)表于 2025-3-29 01:07:07 | 只看該作者
https://doi.org/10.1007/978-3-319-90913-4paleobotany; plant fossils; palynoflora; palynology; paleoecology; paleoclimatology; paleoclimate; paleobio
44#
發(fā)表于 2025-3-29 06:35:20 | 只看該作者
Brazilian Palaeobotany: Past, Present, and Future Perspectives,ses were created. At the end of this period, postgraduate courses were initiated in some universities with a specialization in palaeobotany. In the 1970s, recently graduated palaeobotanists sought new knowledge in European and North American institutions. From then onwards, a continuous partnership
45#
發(fā)表于 2025-3-29 10:16:13 | 只看該作者
46#
發(fā)表于 2025-3-29 15:14:14 | 只看該作者
Plant Diversification Through the Devonian in Brazil,in several institutions was briefly described and illustrated. In total, we compiled 25 genera of fossil plants distributed throughout the Lochkovian–Famennian interval. From the range of genera, three stratigraphic intervals and floral stages were identified, named .-., .-. and .. The early Devonia
47#
發(fā)表于 2025-3-29 16:41:51 | 只看該作者
48#
發(fā)表于 2025-3-29 20:07:24 | 只看該作者
49#
發(fā)表于 2025-3-30 00:43:05 | 只看該作者
Growth Architecture Diversity Among Permian Calamitaleans in Brazil,il suggest a considerable adaptive potential, which is revealed by diversity in both branching and anatomy. Accordingly, variable growth architectures resulted. They are reflected in several new reconstructions established to illustrate how these trees may have looked like. In addition, finds from t
50#
發(fā)表于 2025-3-30 05:15:24 | 只看該作者
,Siliceous Petrifactions in the Permian of the Parnaíba Basin, Central-North Brazil: Sedimentary Envks, anatomically preserved trunks, silcretes, and coquinas are investigated by light and cathodoluminescence microscopy to reveal taphonomic indications. As a result, we provide evidence of similar silicification patterns exhibited by quite different fossils, lithotypes, and host strata, which were
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