Palaeoclimatic inferences based on dendrological patterns of permineralized wood from the Permian of the Northern Tocantins Petrified Forest, Parnaíba Basin, Brazil

Author:

Benício José Rafael Wanderley,Spiekermann Rafael,Manfroi Joseline,Uhl Dieter,Pires Etiene Fabbrin,Jasper AndréORCID

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Geology,Ecology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference57 articles.

1. Almeida, F. F. M., & Carneiro, C. D. R. (2004). Inundações Marinhas Fanerozóicas no Brasil Recursos Minerais Associados. In V. Mantesso-Neto, A. Bartorelli, C. D. R. Carneiro, & B. B. Brito-Neves (Eds.), Geologia do Continente Sul-Americano, Evolução da Obra de Fernando Flávio Marques de Almeida (pp. 43–58). Beca: São Paulo.

2. Borchert, R. (1999). Climatic periodicity, phenology, and cambium activity in tropical dry forest trees. IAWA Journal, 20(3), 239–247.

3. Brea, M. (1998). Análisis de los anillos de crecimiento en leños fósiles de coníferas de la Formación La Meseta, Isla Seymur (Marambio) Antártida. Paleógeno de América de Sur y de la Península Antártida, 5, 163–176.

4. Brison, A. L., Philippe, M., & Thévenard, F. (2001). Are Mesozoic wood growth rings climate induced? Paleobiology, 27(3), 531–538.

5. Capretz, R. L., & Rohn, R. (2013). Lower Permian stems as fluvial paleocurrent indicators of the Parnaíba Basin, northern Brazil. Journal of South American Earth Sciences, 45, 69–82.

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