Wadi Al Dab'i: Late/Upper Maastrichtian, Jordan
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Dinopterygoidea indet.
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Selachia indet.
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"enigmatic tiny 2 mm selachian teeth with three lateral cusplets and broad massive root" | ||||||||||
Cephalopoda
- Ammonitida
- Sphenodiscidae
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Libycoceras acutodorsatus
(Noetling 1897)
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Jagt et al. 2019 | |||||||||
Cephalopoda
- Ammonitida
- Pachydiscidae
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Pachydiscus (Pachydiscus) dossantosi
(Maury 1930)
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Jagt et al. 2019 | |||||||||
Menuites fresvillensis
(Seunes 1890)
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Jagt et al. 2019 | |||||||||
Cephalopoda
- Ammonitida
- Baculitidae
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Baculites sp.
Lamarck 1799
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Jagt et al. 2019 | |||||||||
Baculites ovatus auctorum non Say 1821 | ||||||||||
Bivalvia
- Myalinida
- Inoceramidae
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Tenuipteria ex gr. argentea
(Conrad 1858)
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Jagt et al. 2019 | |||||||||
Reptilia
- Mosasauridae
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Mosasauridae indet.
Gervais 1852
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:new species and genus of small durophagous mosasaurs similar to carinodens" | ||||||||||
Mosasaurus hoffmanni
(Mantell 1829)
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original and current combination Mosasaurus hoffmannii | ||||||||||
Clidastes sp.
Cope 1868
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Liodon anceps
(Owen 1841)
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original and current combination Leiodon anceps | ||||||||||
Tylosaurus indet.
Marsh 1872
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Platecarpus sp.
Cope 1869
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"Platecarpus indet." | ||||||||||
Reptilia
- Testudines
- Cheloniidae
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Gigantatypus salahi n. gen., n. sp.
Kaddumi 2006
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Reptilia
- Plesiosauria
- Polycotylidae
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Polycotylidae indet.
Williston 1908
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Reptilia
- Pterosauria
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Pterosauria indet.
Kaup 1834
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Actinopteri
- Aulopiformes
- Eurypholidae
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Eurypholidae indet.
Goody 1969
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Actinopteri
- Aulopiformes
- Enchodontidae
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Enchodus libycus
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Enchodus elegans
Dartevelle and Casier 1949
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Actinopteri
- Aulopiformes
- Dercetidae
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Stratodus apicalis
Cope 1872
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Dercetis sp.
Agassiz 1834
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Actinopteri
- Ichthyodectiformes
- Ichthyodectidae
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Ichthyodectidae indet.
Crook 1892
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Actinopteri
- Ichthyodectiformes
- Saurodontidae
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Saurocephalus sp.
Harlan 1824
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Saurodon sp.
Hays 1829
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Chondrichthyes
- Myliobatiformes
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Myliobatoidea indet.
()
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Chondrichthyes
- Lamniformes
- Otodontidae
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Cretolamna biauriculate
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Chondrichthyes
- Lamniformes
- Anacoracidae
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Squalicorax pristodontus
(Agassiz 1835)
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see common names |
Geography
Country: | Jordan |
Coordinates: | 31.6° North, 36.5° East (view map) |
Paleocoordinates: | 15.9° North, 30.2° East |
Basis of coordinate: | estimated from map |
Geographic resolution: | local area |
Time
Period: | Cretaceous | Epoch: | Late/Upper Cretaceous |
Stage: | Maastrichtian | 10 m.y. bin: | Cretaceous 8 |
Key time interval: | Late/Upper Maastrichtian | ||
Age range of interval: | 72.10000 - 66.00000 m.y. ago |
Stratigraphy
Formation: | Muwaddar Chalk Marl | ||||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Most vertebrate fossils from lowest stratigraphic zone buried beneath 25 meters of sediments. Menuites fresvillensis is a good index taxon for upper Maastrichtian strata Pachydiscus (P.) dossantosi links Jordan with the (upper) lower to lower upper Maastrichtian in the United Arab Emirates/Oman border area and with more poorly constrained Maastrichtian levels in Brazil and Nigeria. The record of Menuites fresvillensis and sphenodiscids suggests correlation of the MCMF with the Emael and Nekum members of the Maastrichtian Formation (ca 66.5–66.1 Ma), plus the upper part of the coeval Kunrade Formation, in the type area of the Maastrichtian Stage (southeast Netherlands, northeast Belgium). However, associated ‘tegulated’ inoceramids from the MCMF are assignable to the group of Tenuipteria argentea (Conrad, 1858), which corroborates the latest Maastrichtian age of that unit and allows correlation with North America and Europe. |
Lithology and environment
Primary lithology: | lithified marl |
Includes fossils? | Y |
Lithology description: Slightly bituminous light gray chalk marl with very large concretions up to 4 meters in diameter rich in vertebrate remains and also containing secondary Uranium and calcite veins. | |
Environment: | offshore indet. |
Geology comments: The predominantly chalky lithology, coupled with the paucity of any diversified benthic macrofaunal assemblages, the absence of erosional surfaces and the presence of diverse planktonic faunas, indicates a moderate to deep-water pelagic environment (Powell 1989). On the basis of macrofossil evidence at a number of localities, inclusive of sclerorhynchid saw fishes and ginglymostomatid sharks, palaeowater depth is estimated not to have exceeded 100 metres, under prevailing subtropical palaeoclimatic conditions (Kaddumi 2009a). |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Collection excludes: | some macrofossils |
Reason for describing collection: | taxonomic analysis |
Collection method comments: Repository: Eternal River Museum of Natural History (ERMNH) at Amman |
Metadata
Also known as: | Harrana fauna | ||
Database number: | 170239 | ||
Authorizer: | P. Holroyd, M. Clapham | Enterer: | P. Holroyd, M. Clapham |
Modifier: | M. Clapham | Research group: | marine invertebrate,vertebrate |
Created: | 2015-06-17 19:02:59 | Last modified: | 2019-02-12 22:57:05 |
Access level: | the public | Released: | 2015-06-17 19:02:59 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
55540. | H. F. Kaddumi. 2006. A new genus and species of gigantic marine turtles (Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna-Jordan. PalArch Vertebrate Paleontology 2(1):1-14 [P. Holroyd/P. Holroyd] |
Secondary references:
67922 | J. W. M. Jagt, E. A. Jagt-Yazykova, H. F. Kaddumi and J. Lindgren. 2019. Ammonite dating of latest Cretaceous mosasaurid reptiles (Squamata, Mosasauroidea) from Jordan-preliminary observations. Alcheringa 42:587-596 [M. Clapham/M. Clapham/M. Clapham] |