Burma Terrane collision and northward indentation in the Eastern Himalayas recorded in the Eocene‐Miocene Chindwin Basin (Myanmar)
Abstract The Burma Terrane (Myanmar) played an important role in the India‐Asia collision
and moved over 2,000 km northward on the Indian Plate during the Cenozoic, before …
and moved over 2,000 km northward on the Indian Plate during the Cenozoic, before …
Did the Deccan Volcanism impact the Indian flora during the Maastrichtian?
Abstract The Deccan-associated sediments (Lameta Formation and intertrappean) hold
great potential for understanding the role of Deccan Volcanism in the Maastrichtian …
great potential for understanding the role of Deccan Volcanism in the Maastrichtian …
The Cenozoic history of palms: Global diversification, biogeography and the decline of megathermal forests
Aim Megathermal rain forests and mangroves are much smaller in extent today than in the
early Cenozoic, primarily owing to global cooling and drying trends since the Eocene …
early Cenozoic, primarily owing to global cooling and drying trends since the Eocene …
Continental palynomorphs from the Dabaa Formation, North-Western Desert, Egypt: a contribution to the reconstruction of the vegetation on the southern shores of the …
Abstract The Eocene–Oligocene transition period was marked by one of the most abrupt and
severe global environmental changes in the Cenozoic record, and this had a marked …
severe global environmental changes in the Cenozoic record, and this had a marked …
Climate and geological change as drivers of Mauritiinae palm biogeography
G Bogotá‐Ángel, H Huang, PE Jardine… - Journal of …, 2021 - Wiley Online Library
Aim Forest composition and distribution are determined by a myriad of factors, including
climate. As models of tropical rain forest, palms are often used as indicator taxa, particularly …
climate. As models of tropical rain forest, palms are often used as indicator taxa, particularly …
Spinizonocolpites prominatus (McIntyre) Stover & Evans: fossil Nypa pollen, taxonomy, morphology, global distribution, and paleoenvironmental significance
The fossil species Monosulcites prominatus was described from Early Eocene sediments in
Canterbury, New Zealand. It resembles the pollen of the mangrove palm Nypa fruticans …
Canterbury, New Zealand. It resembles the pollen of the mangrove palm Nypa fruticans …
[HTML][HTML] At a crossroads: The late Eocene flora of central Myanmar owes its composition to plate collision and tropical climate
H Huang, D Pérez-Pinedo, RJ Morley… - Review of Palaeobotany …, 2021 - Elsevier
Myanmar was shaped by the India-Asia collision, fusion of the Burma Terrane (BT) with Asia,
and mountain building. Throughout this process new elevational gradients and habitats …
and mountain building. Throughout this process new elevational gradients and habitats …
Sedimentary geochemical records of late Miocene-early Pliocene palaeovegetation and palaeoclimate evolution in the Ying-Qiong Basin, South China Sea
The sedimentary geochemical records of palaeovegetation and palaeoclimate variations in
late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South China Sea have …
late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South China Sea have …
[HTML][HTML] Leaf fossils of Sabalites (Arecaceae) from the Oligocene of northern Vietnam and their paleoclimatic implications
A Song, J Liu, SQ Liang, T Van Do, HB Nguyen, LB Jia… - Plant Diversity, 2022 - Elsevier
Recent paleobotanical investigations in Vietnam provide a good opportunity to improve our
understanding of the biodiversity and paleoclimatic conditions in the geological past of …
understanding of the biodiversity and paleoclimatic conditions in the geological past of …
Late Maastrichtian vegetation and palaeoclimate: palynological inferences from the Deccan Volcanic Province of India
Our understanding of the low latitude terrestrial climate of the late Maastrichtian is far from
satisfactory. We have attempted to reconstruct the late Maastrichtian vegetation and climate …
satisfactory. We have attempted to reconstruct the late Maastrichtian vegetation and climate …