Abstract
A circular structure, 5.5 km in diameter, in central eastern Jordan has been interpreted as a large meteorite impact structure. The age of the Waqf As Suwwan impact is poorly constrained. By examining calcareous nannofossils from the sediments exposed in this structure, an age model of the timing of the event has been obtained. A total of 81 smear slides from two cores (BH-1, BH-2) penetrating the sediments of the central structure were prepared in order to obtain a biostratigraphic age for the post-impact sediments. The calcareous nannofossils assign sediments below the breccias of the core BH-1 an age of late Campanian to late Maastrichtian and a mixture of late Maastrichtian to early Eocene ages in the breccia horizon, while core BH-2 is of early Maastrichtian to late Maastrichtian age. The upper part of the sediments, removed in from adjacent area, consists of breccia components. The presences of calcareous nannofossil marker assemblages suggest that these components were derived from two different sources: a Cretaceous and a Paleocene-Early Eocene one. The deposition of the breccia resulted from gravitational collapse of water-saturated sediments in two stages; the earlier of these was more intensive than the latter. The stratigraphic framework and the presence of reworked Cretaceous and Paleocene calcareous nannofossils within Paleogene nannofossil Zone NP12/NP13 suggests an early Eocene age for the impact. The upper part of the Cretaceous sediments was thermally altered by the impact causing partial or complete dissolution of the calcareous nannofossils. This caused overgrowth for the more resistant species, while others were dissolved.
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Acknowledgments
This study is in cooperation between the American University of Beirut, the Ruhr University Bochum, and the University of Jordan. The University of Jordan hosts the cores. All the analyses were performed in the Ruhr University Bochum and in the Central Research Science Laboratory at the American University of Beirut. The authors would like to thank Dr. Rolf Neuser from the SEM lab of the Department of Geology, Mineralogy and Geophysics (Bochum) for his support. We would like to thank Dr. Jean Self-Trail and Dr. David Watkins for their useful suggestions. We also would like to thank Ms. Ibtisam Baik for her helpful comments. The second author thanks Alexander von Humboldt Foundation (AvH) for their support during his research visit in Museum für Naturkunde.
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Highlights
• Clasts and matrix of the sedimentary breccias were tested.
• The clasts of the breccia were derived from a Paleocene-early Eocene source.
• Material was deposited by gravitational collapses of water-saturated sediments.
• The overgrowth formed on the most resistant taxa during the event.
Appendix
Appendix
Taxonomic list of species have used in this study listed below:
Ahmuellerella Reinhardt
A. octoradiata (Górka) Reinhardt
A. regularis (Górka) Reinhardt and Górka
Arkhangelskiella Vekshina
A. cymbiformis Vekshina
A. maastrichtiana Varol’s
Biscutum Black in Black and Barnes
B. constans (Górka) Black in Black and Barnes
B. ellipticum (Górka) Grün in Grün and Allemann
B. melaniae (Górka) Burnett
Broinsonia Bukry
B. parca (Stradner) Bukry ssp. constricta Hattner et al.
Coccolithus Schwarz
C. pelagicus (Wallich) Schiller
C. formosus (Kamptner) Wise
Cribrosphaerella Deflandre in Piveteau
C. ehrenbergii (Arkhangelsky) Deflandre in Piveteau
Chiasmozygus Gartner
C. bifarius Bukry
Cylindralithus Bramlette and Martini
C. sculptus Bukry
Discoaster Tan
D. barbadiensis Tan
D. binodosus Martini
D. deflandrei Bramlette and Riedel
D. lodoensis Bramlette and Riedel
D. mahmoudii Perch-Nielsen
D. minimus Sullivan
D. multiradiatus Bramlette and Riedel
D. septemradiatus (Klumpp) Martini
Eiffellithus Reinhardt
E. eximius (Stover) Perch-Nielsen
E. gorkae Reinhardt
E. parallelus Perch-Nielsen
Ericsonia Black
E. robusta (Bramlette and Sullivan) Edwards and Perch-Nielsen
Gartnerago Bukry
G. segmentatum (Stover) Thierstein
Girgisia (Bramlette and Sullivan) Voral
G. gammation (Bramlette and Sullivan) Voral
Lithraphidites Deflandre
L. carniolensis Deflandre
L. quadratus Bramlette and Martini
Loxolithus Noël
Loxolithus armilla (Black in Black & Barnes) Noël
Microrhabdulus Deflandre
M. decoratus Deflandre
Micula Vekshina
M. decussata Vekshina
M. murus (Martini) Bukry
M. staurophora (Gardet) Stradner
Micrantholithus Deflandre in Deflandre and Fert
M. speetonensis (Bukry) Perch-Nielsen
Prediscosphaera Vekshina
P. cretacea (Arkhangelsky) Gartner
P. grandis Perch-Nielsen
P. spinosa (Bramlette and Martini) Gartner
Placozygus Hoffman
P. fibuliformis (Reinhardt) Hoffman
Perissocyclus Black
P. fenestratus (Stover) Blak
Petrarhabdus Wind and Wise in Wise
P.copulates (Deflandre) Wind and Wise in Wise
Prinsius Hay and Mohler
P. dimorphosus (Perch-Nielsen) Perch-Nielsen
Reinhardtites Perch-Nielsen
Reinhardtites levis Prins & Sissingh in Sissingh
Retecapsa Black
R. angustiforata Black
R. crenulata (Bramlette and Martini) Grün in Grün and Allemann
Reticulofenestra Hay, Mohler and Wade
R. dictyoda (Deflandre in Deflandre & Fert) Stradner in Stradner & Edward
Rhagodiscus Reinhardt
R. angustus (Stradner) Reinhardt
R. reniformis Perch-Nielsen
Sphenolithus Deflandre in Grassè
S. radians Deflandre in Grassè
S. spiniger Bukry
Tranolithus Stover
T. orionatus (Reinhardt) Reinhardt
T. minimus Bukry
Tortolithus Crux in Crux et al.
T. caistorensis Crux in Crux et al.
Triquetrorhabdulus Martini
T. shetlandensis (Perch-Nielsen) Bown
Thoracosphaera Kamptner
Watznaueria Reinhardt
W. barnesiae (Black) Perch-Nielsen
W. biporta Bukry
W. ovata Bukry
Zeugrhabdotus Reinhardt
Z. noeliae Rood et al.
Z. sigmoides (Bramlette and Sullivan) Bown and Young
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Alqudah, M., Khoury, H., Salameh, E. et al. A story told by calcareous nannofossils—the timing and course of an Eocene meteorite impact in central Jordan. Arab J Geosci 11, 451 (2018). https://doi.org/10.1007/s12517-018-3776-z
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DOI: https://doi.org/10.1007/s12517-018-3776-z