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A unique Late Cretaceous fossil wood assemblage from Chilean Patagonia provides clues to a high-latitude continental environment
Indexado
WoS WOS:001124575800001
Scopus SCOPUS_ID:85179746886
DOI 10.1002/SPP2.1536
Año 2023
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



Fossil plants, including large trunks, stems, some branches, and twigs, were collected from the Maastrichtian (68.9 Ma), upper Dorotea Formation in the Magallanes-Austral Basin, 16 km north of the Cerro Guido-Las Chinas complex in the southern Chilean Magallanes region. These fossil trunks range from 0.2 to 2.2 m in length. Petrographic slides were made in three sections (transverse, radial and tangential) and analysed under a light microscope to study the permineralized fossils. The woods and stems belong to Austroginkgoxylon gen. et sp. nov., Agathoxylon antarcticum, Podocarpoxylon paradoxi sp. nov., Podocarpoxylon mazzonii, Palmoxylon subantarcticae and Notomalvaceoxylon magallanense gen. et sp. nov. The growth rings of gymnosperms and anatomical characters of angiosperms were analysed to obtain palaeoecological data. Interactions between gymnosperm roots growing into the secondary xylem of an angiosperm (nurse logs) are recorded. The data obtained from the fossil woods suggest warm and humid conditions in this southern South American locality during the Late Cretaceous, providing a unique opportunity to study continental environments at high southern latitudes, which are poorly represented on a global scale.

Revista



Revista ISSN
Papers In Palaeontology 2056-2799

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Disciplinas de Investigación



WOS
Paleontology
Scopus
Sin Disciplinas
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Martinez, Leandro C. A. - Museo Histor Reg - Argentina
UNIV NACL LA PLATA - Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas - Argentina
Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata - Argentina
2 LEPPE-CARTES, MARCELO ADRIAN Hombre Instituto Antártico Chileno - Chile
3 Manríquez, Leslie M.E. - Univ Vale Rio dos Sinos - Brasil
Universidade do Vale do Rio dos Sinos - Brasil
3 Manriquez, Leslie M. E. Mujer Univ Vale Rio dos Sinos - Brasil
Universidade do Vale do Rio dos Sinos - Brasil
4 Pino, Juan Pablo Hombre Universidad de Chile - Chile
5 Trevisan, Cristine Mujer Instituto Antártico Chileno - Chile
6 Manfroi, Joseline Mujer Instituto Antártico Chileno - Chile
Corp Invest & Avance Paleontol Hist Nat Atacama CI - Chile
Corporación de Investigación y Avance de La Paleontología e Historia Natural de Atacama – CIAHN Atacama - Chile
7 Mansilla, Héctor Hombre Instituto Antártico Chileno - Chile

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Financiamiento



Fuente
Agencia Nacional de Promoción Científica y Tecnológica
Consejo Nacional de Investigaciones Científicas y Técnicas
Conselho Nacional de Desenvolvimento Científico e Tecnológico
Fondo Nacional de Desarrollo Científico y Tecnológico
CNPq (National Council for Scientific and Technological Development)
Instituto de Botánica Darwinion
INACH (Chilean Antarctic Institute)
Paleogeographic patterns v/s climate change in South America and the Antarctic Peninsula during the latest Cretaceous: a possible explanation for the origin of the Austral biota? (Fondecyt project)
Floras en la transicion Jurasico-Cretacica de la Cuenca Neuquina. Sus implicancias bioestratigraficas y paleoambientales' (Agencia Nacional de Promocion Cientifica y Tecnologica, Argentina
Max Müller
Viviana Lobos
CONICET‐ANCEFN
CONICET-ANCEFN

Muestra la fuente de financiamiento declarada en la publicación.

Agradecimientos



Agradecimiento
We thank Viviana Lobos, Max Mueller, and families from Estancia Cerro Guido for their help and cooperation during fieldwork. We also thank Roberto Pujana, Mariana Brea, Daniela Ruiz and Liliana Mallo (CONICET, Argentina) for their valuable suggestions and literature, which helped us to improve this paper. We are grateful to CNPq (National Council for Scientific and Technological Development), for the Post-Doctoral PhD grant and financial support assistance to JM; to INACH (Chilean Antarctic Institute) for support during the fieldwork; and the Instituto de Botanica Darwinion (CONICET-ANCEFN) for use of the Plant Anatomy Laboratory. This research was supported by Projects 'Paleogeographic patterns v/s climate change in South America and the Antarctic Peninsula during the latest Cretaceous: a possible explanation for the origin of the Austral biota?' (Fondecyt project No. 1151389) and 'Floras en la transicion Jurasico-Cretacica de la Cuenca Neuquina. Sus implicancias bioestratigraficas y paleoambientales' (Agencia Nacional de Promocion Cientifica y Tecnologica, Argentina, PICT-2019-03749). Thanks are given to the two anonymous referees, and to the editor, for their corrections and suggestions that improved the final version of this manuscript.
We thank Viviana Lobos, Max Müller, and families from Estancia Cerro Guido for their help and cooperation during fieldwork. We also thank Roberto Pujana, Mariana Brea, Daniela Ruiz and Liliana Mallo (CONICET, Argentina) for their valuable suggestions and literature, which helped us to improve this paper. We are grateful to CNPq (National Council for Scientific and Technological Development), for the Post‐Doctoral PhD grant and financial support assistance to JM; to INACH (Chilean Antarctic Institute) for support during the fieldwork; and the Instituto de Botánica Darwinion (CONICET‐ANCEFN) for use of the Plant Anatomy Laboratory. This research was supported by Projects ‘Paleogeographic patterns v/s climate change in South America and the Antarctic Peninsula during the latest Cretaceous: a possible explanation for the origin of the Austral biota?’ (Fondecyt project No. 1151389) and ‘Floras en la transición Jurásico‐Cretácica de la Cuenca Neuquina. Sus implicancias bioestratigráficas y paleoambientales’ (Agencia Nacional de Promoción Científica y Tecnológica, Argentina, PICT‐2019‐03749). Thanks are given to the two anonymous referees, and to the editor, for their corrections and suggestions that improved the final version of this manuscript.
We thank Viviana Lobos, Max Müller, and families from Estancia Cerro Guido for their help and cooperation during fieldwork. We also thank Roberto Pujana, Mariana Brea, Daniela Ruiz and Liliana Mallo (CONICET, Argentina) for their valuable suggestions and literature, which helped us to improve this paper. We are grateful to CNPq (National Council for Scientific and Technological Development), for the Post‐Doctoral PhD grant and financial support assistance to JM; to INACH (Chilean Antarctic Institute) for support during the fieldwork; and the Instituto de Botánica Darwinion (CONICET‐ANCEFN) for use of the Plant Anatomy Laboratory. This research was supported by Projects ‘Paleogeographic patterns v/s climate change in South America and the Antarctic Peninsula during the latest Cretaceous: a possible explanation for the origin of the Austral biota?’ (Fondecyt project No. 1151389) and ‘Floras en la transición Jurásico‐Cretácica de la Cuenca Neuquina. Sus implicancias bioestratigráficas y paleoambientales’ (Agencia Nacional de Promoción Científica y Tecnológica, Argentina, PICT‐2019‐03749). Thanks are given to the two anonymous referees, and to the editor, for their corrections and suggestions that improved the final version of this manuscript.

Muestra la fuente de financiamiento declarada en la publicación.