New Early Cretaceous shrimp (Decapoda) from the Sidi Aich Formation of the Northern Chotts Range, southern Tunisia: Taxonomy, biostratigraphy, and palaeoenvironmental implications
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Boukhalfa, Kamel
[1
,3
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Sudarsky, Sergio
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Kent State Univ, Dept Geol, Kent, OH 44242 USAUniv Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
Sudarsky, Sergio
[2
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Ben Ali, Walid
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Univ Tunis El Manar, Fac Sci Tunis, UR11 ES15, Tunis 2092, TunisiaUniv Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
Ben Ali, Walid
[3
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Feldmann, Rodney M.
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Kent State Univ, Dept Geol, Kent, OH 44242 USAUniv Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
Feldmann, Rodney M.
[2
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Schweitzer, Carrie E.
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Kent State Univ Stark, Dept Geol, 6000 Frank Ave NW, North Canton, OH 44720 USAUniv Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
Schweitzer, Carrie E.
[4
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Soussi, Mohamed
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Univ Tunis El Manar, Fac Sci Tunis, UR11 ES15, Tunis 2092, TunisiaUniv Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
Soussi, Mohamed
[3
]
机构:
[1] Univ Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
[2] Kent State Univ, Dept Geol, Kent, OH 44242 USA
[3] Univ Tunis El Manar, Fac Sci Tunis, UR11 ES15, Tunis 2092, Tunisia
[4] Kent State Univ Stark, Dept Geol, 6000 Frank Ave NW, North Canton, OH 44720 USA
The fossil dendrobranchiate shrimp Macropenaeus was originally described from the Upper Cretaceous (Cenomanian) limestones of Hadjoula, northwest Lebanon. A new species, M. sidiaichensis sp. nov., was recovered from the Sidi Aich Formation in the Northern Chotts Range, southern Tunisia. The Barremian occurrence of the genus in Tunisia suggests that Macropenaeus most likely originated in northern Africa and then migrated to Arabia in the Cenomanian. The association of the fossil shrimp with con-chostracans, plant fragments, and fish indicates the interaction of freshwater and marine conditions that characterized the northern African margin as part of widespread coastal complex, paralic environments during the Barremian. (C) 2017 Elsevier Ltd. All rights reserved.