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. 2021 Jun 29;18:34. doi: 10.1186/s12983-021-00418-9

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© The Author(s) 2021

Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated in a credit line to the data.

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Fig. 1 — The changeful history of Italy and its surrounding regions from the mid-Miocene to the Pleistocene. (a) Mid-Miocene (17–16 Ma, the white areas are excluded, black lines show the recent situation), (b) the ‘Lago-Mare’ period (i.e., the first Messinian cycle or the lower gypsum mega-sequence), latest Miocene (6.0–5.6 Ma), (c) Pliocene (5.3–2.6 Ma), (d) Last Glacial Maximum (21 ka), similar distributions of land and sea are also assumed for the previous ice ages of the late Pleistocene. Maps based on Bosellini [12] and Vai [17]