Continental Triassic sequences in Antarctica are among the most continuous and best represented in Gondwana. Triassic fossil plants have been collected sporadically from Antarctica since the beginning of the twentieth century, but our knowledge of the vegetation during this time has dramatically increased during the last three decades. Here we review the fossil record of Triassic plants as representatives of natural groups from sites along the Transantarctic Mountains, using the fossils as evidence for successive vegetational changes through the Triassic, taking into account that these plant communities were living under particular high-latitude (706 or higher) paleoclimatological conditions, including a polar light regime. Even though our ...
Abstract The mass extinction at the Permian-Triassic boundary produced a floral turnover in Gondwana...
David.J. Cantrill and Imogene PooleCambridge University Press, Cambridge, 2012. ISBN 978−0−521−85598...
This is the publisher's version, which is also available electronically from: http://dx.doi.org/10.4...
International audiencePremise of research.Well-preserved Triassic plant fossils from Antarctica yiel...
Premise of research. Well-preserved Triassic plant fossils from Antarctica yield insights into the p...
Premise of research. Well-preserved Triassic plant fossils from Antarctica yield insights into the p...
Compared with the fossil record of vascular plants, bryophyte fossils are rare; this cir-cumstance i...
Nowadays the Antarctic continent is almost entirely covered by ice (around 98% of the total land sur...
Throughout Earth history, plants were apparently less dramatically affected by global biotic crises ...
International audienceDuring the ␣rst Korea Antarctic Geological Expedition (KAGEX I, 2013/2014), fo...
New collections of plant material from the Merrick and Sweeney Mountains provide further evidence of...
The Permian-Triassic boundary within the Amery Group of the Lambert Graben is placed at the contact ...
This is the publisher's version, which has been shared with permission. The original version may be ...
Study of the Triassic floristic record of several stratigraphic units of southern and west‐central A...
A Triassic macrofloral assemblage is documented from the Quebrada de los Fósiles Formation, lower un...
Abstract The mass extinction at the Permian-Triassic boundary produced a floral turnover in Gondwana...
David.J. Cantrill and Imogene PooleCambridge University Press, Cambridge, 2012. ISBN 978−0−521−85598...
This is the publisher's version, which is also available electronically from: http://dx.doi.org/10.4...
International audiencePremise of research.Well-preserved Triassic plant fossils from Antarctica yiel...
Premise of research. Well-preserved Triassic plant fossils from Antarctica yield insights into the p...
Premise of research. Well-preserved Triassic plant fossils from Antarctica yield insights into the p...
Compared with the fossil record of vascular plants, bryophyte fossils are rare; this cir-cumstance i...
Nowadays the Antarctic continent is almost entirely covered by ice (around 98% of the total land sur...
Throughout Earth history, plants were apparently less dramatically affected by global biotic crises ...
International audienceDuring the ␣rst Korea Antarctic Geological Expedition (KAGEX I, 2013/2014), fo...
New collections of plant material from the Merrick and Sweeney Mountains provide further evidence of...
The Permian-Triassic boundary within the Amery Group of the Lambert Graben is placed at the contact ...
This is the publisher's version, which has been shared with permission. The original version may be ...
Study of the Triassic floristic record of several stratigraphic units of southern and west‐central A...
A Triassic macrofloral assemblage is documented from the Quebrada de los Fósiles Formation, lower un...
Abstract The mass extinction at the Permian-Triassic boundary produced a floral turnover in Gondwana...
David.J. Cantrill and Imogene PooleCambridge University Press, Cambridge, 2012. ISBN 978−0−521−85598...
This is the publisher's version, which is also available electronically from: http://dx.doi.org/10.4...