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ꯁꯟꯗꯣꯛꯅꯥ ꯇꯥꯛꯄꯥDire Straits FIG 01.jpg
English: Palaeogeographical reorganization of the Tethys–Paratethys region during the Paleogene, from a connected Tethys configuration during the early Eocene (a) to a fragmented and restricted Paratethys region configuration during the Oligocene (b). Note the loss of deep-water connections between the Indian Ocean region and the Mediterranean, the complete loss of Indian–Arctic Ocean connections, and the closure of most of the Eocene seaways in the Oligocene time.
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ꯍꯧꯔꯛꯐꯛ Palcu, D. V & Krijgsman, W. The dire straits of Paratethys: gateways to the anoxic giant of Eurasia. Geol. Soc. London, Spec. Publ. 523, SP523-2021–73 (2023). doi:10.1144/SP523-2021-73
ꯄꯨꯊꯣꯛꯂꯤꯕ ꯃꯤ Dan.palcu

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Palaeogeographical reorganization of the Tethys–Paratethys region during the Paleogene, from a connected Tethys configuration during the early Eocene (above) to a fragmented and restricted Paratethys region configuration during the Oligocene (below).

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