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Palynological Investigations of the Miocene sediments from Murree formation of Pakistan: Evidence for Palaeoenvironment and Palaeoclimate interpretations. | LitMetric

AI Article Synopsis

  • The study focused on analyzing the palynoflora of the Murree formation to explore how climate and vegetation have changed over time using microscope techniques.
  • A total of 31 samples were examined, identifying a variety of palynomorphs, with Asteraceae as the most dominant family and notable findings including the genus Pinus.
  • The research highlighted the importance of angiosperms, especially noting their abundance in the Miocene epoch, and emphasized how Holocene samples can provide insights into the area's vegetation origins and environmental changes.

Article Abstract

The present study was carried out to investigate the palynoflora of Murree formation using microscopic techniques to understand the climatic changes and vegetation's evolution. In this palynological study, 31 samples were collected, analyzed, and then identified as palynomorphs using different previous published literature. The results of this study will be described in terms of the evolutionary history of plants and the depositional environment of the reported taxa in the study area. The botanical affinities and systematic description of the taxa were examined using light and scanning electron microscopy. The floral record identified Asteraceae as the dominant family and Pinus as a genus. Most of angiosperms i.e Fabaceae and Poaceae, have a poor fossil record but have an abundant palynological record in the study area. The highest polar diameter (75.75 μm), colpus length (34.5 μm) and colpus width (31 μm) were examined for the Convolvulus. Most of the taxa explained here had a wide geographical occurrence in Southeast Asia and show the abundance of angiosperms in the Miocene epoch. The palynological record of Holocene samples is important to know about the vegetation's origin and environmental fluctuations in the study area.

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Source
http://dx.doi.org/10.1590/0001-3765202420231241DOI Listing

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