2016
DOI: 10.1016/j.quaint.2015.08.067
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Did the Red Sea – Mediterranean connection over the Dead Sea Fault Zone end in the Late Pliocene?

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Cited by 7 publications
(2 citation statements)
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“…One of the most invasive alien foraminifer species, Amphistegina lobifera , was found in the core materials from Mersin (Turkey), dated back to 227.3 ± 17.8, ka BP [ 46 ]. Some Indo-Pacific foraminifer species were also found together with the Mediterranean species in the Quaternary sediments collected from the Asi River (Orontes) Delta [ 47 ]. It was suggested that these species might have been introduced to the Eastern Mediterranean much before the opening of the Suez Canal.…”
Section: Resultsmentioning
confidence: 99%
“…One of the most invasive alien foraminifer species, Amphistegina lobifera , was found in the core materials from Mersin (Turkey), dated back to 227.3 ± 17.8, ka BP [ 46 ]. Some Indo-Pacific foraminifer species were also found together with the Mediterranean species in the Quaternary sediments collected from the Asi River (Orontes) Delta [ 47 ]. It was suggested that these species might have been introduced to the Eastern Mediterranean much before the opening of the Suez Canal.…”
Section: Resultsmentioning
confidence: 99%
“…Furthermore, during the Middle-Late Pliocene, an eastern Mediterranean-Red Sea connection was established through the Gulf of Aqaba on the Dead Sea Fault Zone (Popov et al, 2006). Meriç et al (2016) showed that this connection was maintained until the Late Pleistocene, and therefore offers another possible explanation for the large abundance of cosmopolitan fish in the eastern Mediterranean. It may also explain the complete extinction of typical Miocene-Pliocene species that had remained until that time, whose extant closest relatives however are not found today in the Mediterranean, such as…”
Section: Mediterrranean Teleost Fish Paleobiogeographic Distributionmentioning
confidence: 97%