Open Access Open Access  Restricted Access Subscription Access

Neogene Climate Evolution in Eurasia


Affiliations
1 Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
 

The third Neogene Climate Evolution in Eurasia (NECLIME) Asian meet aimed to reconstruct the palaeoclimate using a multiproxy approach, viz. megafossils (plants, vertebrates and invertebrates), microfossils (pollen-spores, phytoliths, diatoms, forams, nanofossils, etc.), isotopes, geological and geochemical signals. The meeting also provided an opportunity to enhance the database of low-latitudinal area of Eurasia, where monsoon pattern is considered as an important factor for floral and faunal evolution and their biodiversity. The major themes covered in the meeting included palaeobiogeography and biodiversity, climate and fauna, palaeoclimatic reconstruction as well as climate and vegetation dynamics of Neogene and Quaternary time.
User
Notifications
Font Size

Abstract Views: 365

PDF Views: 153




  • Neogene Climate Evolution in Eurasia

Abstract Views: 365  |  PDF Views: 153

Authors

Ipsita Roy
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Shazi Farooqui
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Syed Azharuddin
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India

Abstract


The third Neogene Climate Evolution in Eurasia (NECLIME) Asian meet aimed to reconstruct the palaeoclimate using a multiproxy approach, viz. megafossils (plants, vertebrates and invertebrates), microfossils (pollen-spores, phytoliths, diatoms, forams, nanofossils, etc.), isotopes, geological and geochemical signals. The meeting also provided an opportunity to enhance the database of low-latitudinal area of Eurasia, where monsoon pattern is considered as an important factor for floral and faunal evolution and their biodiversity. The major themes covered in the meeting included palaeobiogeography and biodiversity, climate and fauna, palaeoclimatic reconstruction as well as climate and vegetation dynamics of Neogene and Quaternary time.


DOI: https://doi.org/10.18520/cs%2Fv111%2Fi11%2F1743-1744