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. 2022 Jan 27;12:1518. doi: 10.1038/s41598-022-05257-0

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© The Author(s) 2022

Open Access This 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/.

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Global distribution of the subfamily Parreysiinae and tectonic plate boundaries. The subfamily range based on available published sources^23,239 and our own data. The red lines indicate tectonic plate boundaries²⁴⁰. The red abbreviations indicate the names of larger tectonic plates: AF African; AM Amurian; AN Antarctic; AR Arabian; AT Anatolian; AU Australian; CL Caroline; IN Indian; NA North American; OK Okinawa; PS Philippine Sea Plate; SO Somalia; SU Sunda (with Indochina Block and Sibumasu Terrane); YA Yangtze. The boundaries of the Burma Terrane (BT), Sibumasu Terrane (ST), Indochina Block (IB), and the Andaman Platelet (AP) are given based on a series of modern tectonic works^38–40. The Mogok–Mandalay–Mergui Belt⁴⁰ is placed here within the boundary of the Burma Terrane. The map was created using ESRI ArcGIS 10 software (https://www.esri.com/arcgis). The topographic base of the map was created with Natural Earth Free Vector and Raster Map Data (https://www.naturalearthdata.com) and Global Self-consistent Hierarchical High-resolution Geography (https://www.soest.hawaii.edu/wessel/gshhg). (Map: Mikhail Yu. Gofarov).