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Rodolphe Tabuce - One of the best experts on this subject based on the ideXlab platform.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
Sylvain Adnet - One of the best experts on this subject based on the ideXlab platform.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
Henri Cappetta - One of the best experts on this subject based on the ideXlab platform.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
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a middle late eocene vertebrate fauna marine fish and mammals from southwestern morocco preliminary report age and palaeobiogeographical implications
Geological Magazine, 2010Co-Authors: Sylvain Adnet, Henri Cappetta, Rodolphe TabuceAbstract:Recent field work in the southern Moroccan Sahara (‘Western Sahara’), south of the city of ad-Dakhla, has led to the discovery of several new fossiliferous sites with fossil vertebrates in sedimentary deposits previously reported for the Mio-Pliocene. The sedimentology and geological setting of the studied area are briefly reported here, and at least three units have been identified in successive stratigraphical sequences according to their fossil content. The first preliminary list of vertebrate associations is reported and consists mainly of isolated teeth belonging to selachian and bony fishes, a proboscidean tooth currently assigned to ? Numidotherium sp. and many remains of archaeocete whales (Basilosauridae). At least 48 species of selachians are presently identified; many of them are new and others are recorded in the late Middle Eocene (Bartonian) and Late Eocene (Priabonian) of Wadi Al-Hitan (Egypt) or Wadi Esh-Shallala Formation (Jordan) as in other African localities (e.g. Otodus cf. sokolowi, ‘Cretolamna’ twiggsensis, Xiphodolamia serrata, Misrichthys stromeri, Hemipristis curvatus, Galeocerdo cf. eaglesomi, Propristis schweinfurthi ), probably indicating a Late Eocene age for unit 2 of the bedrock successions. The evolutionary trend noticeable on the proboscidean tooth is in agreement with such an assumption, by comparison with the close relative species known from the Eocene of Egypt, Libya and Algeria. Indeed, the faunal associations from the Dakhla area clearly demonstrate the erroneous age of these deposits, previously thought to be Mio-Pliocene. It suggests a correlation in age (late Middle Eocene–Late Eocene) and a similar environment with the famous marine deposits from Egypt and Jordan. It opens new opportunities to understand the biogeography and the surprising similarity of landscape between West and Northeast Africa during the Bartonian–Priabonian period.
Albert E. Sanders - One of the best experts on this subject based on the ideXlab platform.
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a new protocetid whale cetacea archaeoceti from the late middle eocene of south carolina
American Museum Novitates, 2005Co-Authors: Jonathan H. Geisler, Albert E. SandersAbstract:A new genus and species of protocetid cetacean, Carolinacetus gingerichi, is described from a partial skull, the posterior portion of both dentaries, 13 vertebrae, and elements of 15 ribs found in the Cross Member of the late middle Eocene Tupelo Bay Formation in Berkeley County, South Carolina. That formation is also defined and named in this paper. Although the holotype skull of Carolinacetus is fragmentary, it includes the best preserved petrosal of any described specimen from the archaeocete families of Pakicetidae, Ambulocetidae, Remingtonocetidae, and Protocetidae. The phylogenetic relationships of Carolinacetus were determined by a cladistic analysis of a dataset that includes 16 cetacean taxa and 5 outgroups scored for 107 morphological characters. Carolinacetus was found to be the basalmost cetacean known from North America, and the most conspicuous character supporting this position is the external, bony nares being anterior to P1. Other noteworthy findings are that Georgiacetus is more basal than Babiacetus and that Remingtonocetidae occupies a branch between Pakicetidae and Protocetidae. Based on our phylogenetic analysis, the genus Gaviacetus is removed from the Basilosauridae and restored to the Protocetidae. Possible dispersal routes of protocetids from the Old World to the New World are discussed, and a route westward along the southern coast of Greenland is considered to be the most likely avenue of protocetid migration to North America.
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A new protocetid whale (Cetacea: Archaeoceti) from the late middle Eocene of South Carolina
American Museum Novitates, 2005Co-Authors: Jonathan H. Geisler, Albert E. Sanders, Zhe-xi LuoAbstract:A new genus and species of protocetid cetacean, Carolinacetus gingerichi, is described from a partial skull, the posterior portion of both dentaries, 13 vertebrae, and elements of 15 ribs found in the Cross Member of the late middle Eocene Tupelo Bay Formation in Berkeley County, South Carolina. That formation is also defined and named in this paper. Although the holotype skull of Carolinacetus is fragmentary, it includes the best preserved petrosal of any described specimen from the archaeocete families of Pakicetidae, Ambulocetidae, Remington-ocetidae, and Protocetidae. The phylogenetic relationships of Carolinacetus were determined by a cladistic analysis of a dataset that includes 16 cetacean taxa and 5 outgroups scored for 107 morphological characters. Carolinacetus was found to be the basalmost cetacean known from North America, and the most conspicuous character supporting this position is the ex-ternal, bony nares being anterior to P1. Other noteworthy findings are that Georgiacetus is more basal than Babiacetus and that Remingtonocetidae occupies a branch between Pakice-tidae and Protocetidae. Based on our phylogenetic analysis, the genus Gaviacetus is removed from the Basilosauridae and restored to the Protocetidae. Possible dispersal routes of proto
Ewan R Fordyce - One of the best experts on this subject based on the ideXlab platform.
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an archaeocete whale cetacea archaeoceti from the eocene waihao greensand new zealand
Journal of Vertebrate Paleontology, 1997Co-Authors: Richard Kohler, Ewan R FordyceAbstract:ABSTRACT An incomplete skull, four vertebrae, two teeth, and other, smaller fragments confirm the early occurrence of dorudontine whales (Cetacea: Archaeoceti: Basilosauridae) in the Southwest Pacific. This material, which is tentatively identified as Zygorhiza sp., (Dorudontinae), derives from the early Bartonian part of the Waihao Greensand, a marine, glauconitic, muddy sandstone. These New Zealand fossils provide one of the oldest records for the Dorudontinae and the oldest reported cetacean for the Southern Hemisphere. Other supposed cetacean records for the Southern Hemisphere are of Priabonian age from Seymour Island, Antarctica. The New Zealand material provides a significant range extension for the Dorudontinae, which previously have been reported from early Lutetian, middle to late Bartonian, and mainly Priabonian strata of the Northern Hemisphere.