1993
DOI: 10.1080/09397140.1993.10637638
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A preliminary correlation between the plio-pleistocene malacofaunas of the Jordan Valley (Israel) and the Orontes Valley (Syria)

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Cited by 16 publications
(7 citation statements)
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“…From Upper Pliocene layers of the Yarmouk outlet Picard (1934; plate 8, figs 15–27) described a fossil species, Melanopsis turriformis , as having a high number of ribs as compared to costata . Later, Schütt & Ortal (1993; plate 2, figs 19, 20) illustrated shells from ‘Ubeidiya which they suggested were M. t. turriformis. No measurements were given for these specimens but they seem to us so similar to costata that we consider them synonyms.…”
Section: Resultsmentioning
confidence: 99%
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“…From Upper Pliocene layers of the Yarmouk outlet Picard (1934; plate 8, figs 15–27) described a fossil species, Melanopsis turriformis , as having a high number of ribs as compared to costata . Later, Schütt & Ortal (1993; plate 2, figs 19, 20) illustrated shells from ‘Ubeidiya which they suggested were M. t. turriformis. No measurements were given for these specimens but they seem to us so similar to costata that we consider them synonyms.…”
Section: Resultsmentioning
confidence: 99%
“…No measurements were given for these specimens but they seem to us so similar to costata that we consider them synonyms. In the material of ‘Ubeidiya (layer II‐36) we measured shells labelled by Schütt & Ortal (1993) as turriformis and compared them to shells labelled by them as costata from the same layer. No significant differences were found.…”
Section: Resultsmentioning
confidence: 99%
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“…Extinct species of Viviparidae occur in the Pleistocene coquina beds along the rivers Jordan in Israel and Orontes in Syria (Kinzelbach 1980; Schütt & Ortal 1993). The coquina beds in the Upper Jordan Valley were defined by Picard (1963) as the Viviparus beds of the GBY Formation with the index fossil Viviparus apameae (Blanckenhorn).…”
mentioning
confidence: 99%