Version 1
: Received: 6 May 2023 / Approved: 8 May 2023 / Online: 8 May 2023 (09:49:27 CEST)
Version 2
: Received: 26 May 2023 / Approved: 29 May 2023 / Online: 29 May 2023 (08:10:16 CEST)
Version 3
: Received: 31 May 2023 / Approved: 1 June 2023 / Online: 1 June 2023 (05:08:18 CEST)
Pazonyi, P.; Szentesi, Z.; Mészáros, L.; Hír, J.; Gasparik, M. Stratigraphic and Paleoecological Significance of the Early/Middle Pleistocene Vertebrate Fauna of the Süttő 21 Site. Diversity2023, 15, 736.
Pazonyi, P.; Szentesi, Z.; Mészáros, L.; Hír, J.; Gasparik, M. Stratigraphic and Paleoecological Significance of the Early/Middle Pleistocene Vertebrate Fauna of the Süttő 21 Site. Diversity 2023, 15, 736.
Pazonyi, P.; Szentesi, Z.; Mészáros, L.; Hír, J.; Gasparik, M. Stratigraphic and Paleoecological Significance of the Early/Middle Pleistocene Vertebrate Fauna of the Süttő 21 Site. Diversity2023, 15, 736.
Pazonyi, P.; Szentesi, Z.; Mészáros, L.; Hír, J.; Gasparik, M. Stratigraphic and Paleoecological Significance of the Early/Middle Pleistocene Vertebrate Fauna of the Süttő 21 Site. Diversity 2023, 15, 736.
Abstract
The Süttő 21 site is a fissure fill of the freshwater limestone of the Gazda quarry in Süttő. The material was collected between 2017 and 2019, the results are summarised in this article, with a special focus on the small vertebrate fauna of the site and its stratigraphic and paleoecological significance.
The fissure fill can be placed around the early/middle Pleistocene boundary (ca. 1.1 and 0.77 Ma). The paleoecological analysis of the herpeto- and mammal fauna of the sequence indicates the proximity of a permanent water body. The lower part of the sequence is dominated by open habitat indicator taxa indicating a cool, dry climate. Towards the upper part of the sequence, the climate remained cool but became wetter, and the vegetation gradually changed to forest-steppe/open forest.
The fauna of the Süttő 21 site can be compared with the material of sites, which are of similar age, thus revealing taxonomic and paleoecological differences between different areas of the country. While a warm, dry climate and open vegetation can be reconstructed in the Villány Hills around the early/middle Pleistocene boundary, the northern Hungarian areas had a cooler, wetter climate, and slightly more closed (grove, forest-steppe) vegetation during this period.
Keywords
vertebrate fauna; paleoecology; stratigraphy; early and middle Pleistocene
Subject
Environmental and Earth Sciences, Paleontology
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
