4.3 Article

Palaeoenvironmental reconstruction of the late Miocene macroflora of La Bisbal d'Emporda (Catalonia, Spain). Comparison with small mammals

期刊

出版社

ELSEVIER
DOI: 10.1016/j.revpalbo.2021.104583

关键词

Neogene; Riverine vegetation; Taphonomy; Paleoecology; Micromammals; South Europe

资金

  1. Spanish Research Agency (AEI) [PID2020-113912GB-100 / AEI / 10.13039/501100011033, PID2020-117289GB-100 / AEI /10.13039/501100011033]
  2. European Regional Development Fund (ERDF) [PID2020-113912GB-100 / AEI / 10.13039/501100011033, PID2020-117289GB-100 / AEI /10.13039/501100011033]
  3. AGAUR (Research Agency of the Catalan Autonomous Government) [2017 SGR 824, 2017 SGR 116]
  4. Spanish Ministry of Economy and Competitiveness (MINECO) [RYC-2013-12470]

向作者/读者索取更多资源

The study of the late Miocene flora from La Bisbal d'Emporda in Catalonia, Spain, provides insights into coastal vegetation in the north-eastern Iberian Peninsula during a key period of Neogene climatic evolution. By re-examining a historical leaf collection and comparing it with data from the associated small mammal fauna, the research highlights the diverse plant assemblages and their ecological implications for the local environment. The findings suggest a more heterogeneous environment than previously thought, with riverine processes influencing the flora and limiting climatic conclusions derived from leaf physiognomic analyses.
The late Miocene flora from La Bisbal d'Emporda (Catalonia, Spain) provides significant data for characterising the coastal vegetation from the north-eastern Iberian Peninsula during a key period in Neogene climatic evolution. To this end, a historical leaf collection from La Bisbal d'Emporda was re-examined, analysed from a palaeoenvironmental viewpoint and compared with data provided by the associated small mammal fauna. This flora dates from 9.6-9.7 Ma in age (early Tortonian) according to small mammal biostratigraphy. The fossil-bearing beds were deposited in the floodplain of a meandering river system. Three palaeoecological assemblages were recognized: 1) Helophytic plant stems related to a wetland community. 2) Torn leaves of Fraxinus sp, Litmus sp, Zelkova sp., Cedrelospermum sp. Populus balsamoides, Alnus gaudinii, Carpinus sp., Platanus sp., Acer tricuspidatum, Daphnogene sp. and, Laurophyllum sp. which would have belonged to a riparian forest located beyond the wetland community, with Fraxinus being the plant growing in closest proximity; 3) Isolated complete Paliurus seeds, interpreted as mainly wind-transported, which provide evidence of an open and more arid landscape situated distally from the floodplain. The small mammal assemblages associated with this flora are consistent with this palaeoenvironmental interpretation. The paucity of small arboreal mammal taxa and insectivores suggests limited forested vegetation areas, while the more common terrestrial species indicate better developed open landscapes. Our results show a more heterogeneous environment than previously thought and that the riverine processes impinged the flora, somewhat limiting the climatic conclusions that might be derived from leaf physiognomic analyses such as CLAMP. (C) 2021 Elsevier B.V. All rights reserved.

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