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Volume 29 Issue 4
Jul 2018
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Article Contents
Hendrik Nowak, Elke Schneebeli-Hermann, Evelyn Kustatscher. Correlation of Lopingian to Middle Triassic Palynozones. Journal of Earth Science, 2018, 29(4): 755-777. doi: 10.1007/s12583-018-0790-8
Citation: Hendrik Nowak, Elke Schneebeli-Hermann, Evelyn Kustatscher. Correlation of Lopingian to Middle Triassic Palynozones. Journal of Earth Science, 2018, 29(4): 755-777. doi: 10.1007/s12583-018-0790-8

Correlation of Lopingian to Middle Triassic Palynozones

doi: 10.1007/s12583-018-0790-8
Funds:

the Euregio Science Fund (call 2014, IPN16:"The end-Permian mass extinction in the Southern and Eastern Alps:extinction rates vs taphonomic biases in different depositional environments") of the Europaregion/Euregio Tirol-Südtirol-Trentino/Tirolo-Alto Adige-Trentino 

SYNTHESYS (access call 4, 2016, GB-TAF-6751:"Diversity changes of spores and pollen during the Permian-Triassic mass extinction") 

More Information
  • Corresponding author: Hendrik Nowak
  • Received Date: 17 Jan 2018
  • Accepted Date: 28 Apr 2018
  • Publish Date: 01 Aug 2018
  • Terrestrial floras underwent important changes during the Lopingian (Late Permian), Early Triassic, and Middle Triassic, i.e., before, during, and after the end-Permian mass extinction. An accurate account of these developments requires reliable correlation. Macrofossils of land plants can only provide a low-resolution biostratigraphy, while detailed zonation schemes based on palynomorphs are available for many regions. Their applicability is still limited due to several factors, such as (micro-)floral provincialism, a lack of suitable marker taxa commonly occurring at important boundaries, and in many cases a lack of independent age control. Nevertheless, these paly-nostratigraphic schemes are regularly used for dating and correlation of successions between differ-ent regions. To support such efforts, the biozonation schemes based on palynomorphs from the Lop-ingian up to and including the Middle Triassic from across the world are summarized and revised. Thus, a consistent correlation of palynozones with the currently recognized international stages is established.

     

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