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Adaffa Formation

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Journal Article
Published: 11 June 2008
Geological Magazine (2008) 145 (5): 648–654.
...B. P. KEAR; T. H. RICH; M. A. ALI; Y. A. AL-MUFARRIH; A. H. MATIRI; A. M. MASARY; Y. ATTIA Abstract Marine reptile remains occur in the Upper Cretaceous (lower Campanian to lower Maastrichtian) Adaffa Formation of NW Saudi Arabia. This is the first detailed report of late Mesozoic marine reptiles...
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Chelonian and crocodyliform remains from the Adaffa Formation of Saudi Arabia. (a) Bothremydid plastron fragment with highlighted inter-plate suture (SGS 004-10) in ventral view. Bothremydid right femur (SGS 006-84): (b) ventral; (c) lateral; (d) dorsal views. Crocodyliform cranial fragment (SGS 004-32): (e) dorsal; (f) ventral views. Dyrosaurid cervical centrum (SGS 006-204): (g) lateral; (h) anterior views. Dyrosaurid dorsal centrum (SGS 006-16): (i) lateral; (j) anterior views. Scale bar represents 30 mm in (a–d) and 20 mm in (e–j).
Published: 11 June 2008
Figure 2. Chelonian and crocodyliform remains from the Adaffa Formation of Saudi Arabia. (a) Bothremydid plastron fragment with highlighted inter-plate suture (SGS 004-10) in ventral view. Bothremydid right femur (SGS 006-84): (b) ventral; (c) lateral; (d) dorsal views. Crocodyliform cranial
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Plesiosaur remains from the Adaffa Formation of Saudi Arabia. Elasmosaurid skull rostrum and mandibular symphysis (SGS 006-20): (a) dorsal; (b) ventral; (c) right lateral views. Abbreviations: adt – anterior dentary teeth; apts – anterior premaxillary tooth sockets; asm – approximate snout midline; def – dentary fang; den – dentary; enr – external naris region; ino? – possible internal narial opening; max – maxilla; msm – median symphysis midline; mxf – maxillary fang; orb – orbit; pmx – premaxilla; rp-ms – reconstructed premaxillary-maxillary suture; vom – vomer. Scale bars represent 50 mm.
Published: 11 June 2008
Figure 3. Plesiosaur remains from the Adaffa Formation of Saudi Arabia. Elasmosaurid skull rostrum and mandibular symphysis (SGS 006-20): (a) dorsal; (b) ventral; (c) right lateral views. Abbreviations: adt – anterior dentary teeth; apts – anterior premaxillary tooth sockets; asm – approximate
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Aquatic squamate remains from the Adaffa Formation of Saudi Arabia. (a) Prognathodon teeth (SGS 006-217) in labial and apical (bottom right) views. Mosasaurid pygal vertebra (SGS 006-542): (b) anterior; (c) posterior views. Indeterminate small varanoid dorsal vertebra (SGS 004-70): (d) dorsal; (e) anterior; (f) left lateral; (g) posterior views. Plioplatecarpine mosasaurid dorsal vertebra (SGS 006-340): (h) anterior; (i) lateral; (j) posterior views. Scale bar represents 30 mm in (a, h–j), 50 mm in (b, c) and 10 mm in (d–g).
Published: 11 June 2008
Figure 4. Aquatic squamate remains from the Adaffa Formation of Saudi Arabia. (a) Prognathodon teeth (SGS 006-217) in labial and apical (bottom right) views. Mosasaurid pygal vertebra (SGS 006-542): (b) anterior; (c) posterior views. Indeterminate small varanoid dorsal vertebra (SGS 004-70
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Sandstones and shales of the Upper Cretaceous Adaffa Formation (Suqah Group); Aynunah Graben, Midyan Basin (28°05′45″N, 35°16′3.4″E). See Figure 1a for location.
Published: 01 July 2005
Figure 6: Sandstones and shales of the Upper Cretaceous Adaffa Formation (Suqah Group); Aynunah Graben, Midyan Basin (28°05′45″N, 35°16′3.4″E). See Figure 1a for location.
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Conglomerates and sandstones of the Adaffa Formation note iron staining (arrow). Located at 28°05′48.5″N, 35°16′02.6″E; view looking north. Width of photo about 12 m.
Published: 01 July 2005
Figure 7: Conglomerates and sandstones of the Adaffa Formation note iron staining (arrow). Located at 28°05′48.5″N, 35°16′02.6″E; view looking north. Width of photo about 12 m.
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Iron-stained, cross-bedded sandstones of the Adaffa Formation (Suqah Group); Midyan Basin (28°05′48.5″N, 35°16′02.6″E). These sediments contain petrified wood, phosphatic nodules and fossilized dinosaur bones.
Published: 01 July 2005
Figure 8: Iron-stained, cross-bedded sandstones of the Adaffa Formation (Suqah Group); Midyan Basin (28°05′48.5″N, 35°16′02.6″E). These sediments contain petrified wood, phosphatic nodules and fossilized dinosaur bones.
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Variegated shales in the Adaffa Formation (Suqah Group), Midyan Basin, located at 28°05′53.6″N, 35°16′16.7″E.
Published: 01 July 2005
Figure 9: Variegated shales in the Adaffa Formation (Suqah Group), Midyan Basin, located at 28°05′53.6″N, 35°16′16.7″E.
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Sands from weathered Adaffa Formation (Suqah Group) outcrops forming low hills within the southern part of the Midyan Basin; exposed in the Aynunah Graben, 11 km north of Al Khuraybah (28°05′46.5″N, 35°16′07.4″E).
Published: 01 July 2005
Figure 12: Sands from weathered Adaffa Formation (Suqah Group) outcrops forming low hills within the southern part of the Midyan Basin; exposed in the Aynunah Graben, 11 km north of Al Khuraybah (28°05′46.5″N, 35°16′07.4″E).
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Sandstones and shales of the Upper Cretaceous Adaffa formation as exposed in the Aynunah graben (28°05'45"N; 35°16'3.4"E).
Published: 01 October 1999
Figure 8: Sandstones and shales of the Upper Cretaceous Adaffa formation as exposed in the Aynunah graben (28°05'45"N; 35°16'3.4"E).
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2005
GeoArabia (2005) 10 (3): 49–126.
...Figure 6: Sandstones and shales of the Upper Cretaceous Adaffa Formation (Suqah Group); Aynunah Graben, Midyan Basin (28°05′45″N, 35°16′3.4″E). See Figure 1a for location. ...
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First thumbnail for: Lithostratigraphy of the Red Sea Region
Second thumbnail for: Lithostratigraphy of the Red Sea Region
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1999
GeoArabia (1999) 4 (4): 503–542.
...Figure 8: Sandstones and shales of the Upper Cretaceous Adaffa formation as exposed in the Aynunah graben (28°05'45"N; 35°16'3.4"E). ...
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Cobbles and pebbles of chert and phosphatic nodules within the Adaffa Formation (Suqah Group), Midyan Basin (28°05′48.5″N, 35°16′02.6″E).
Published: 01 July 2005
Figure 10: Cobbles and pebbles of chert and phosphatic nodules within the Adaffa Formation (Suqah Group), Midyan Basin (28°05′48.5″N, 35°16′02.6″E).
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Bone fragments (upper two specimens) and freshwater turtle carapace found within the Adaffa Formation (Suqah Group), south Midyan Basin. Identified as from a sauropod dinosaur, possibly a titanosaurid (written communication from Dr. P. Whybrow, Natural History Museum, London; June 9, 1993).
Published: 01 July 2005
Figure 11: Bone fragments (upper two specimens) and freshwater turtle carapace found within the Adaffa Formation (Suqah Group), south Midyan Basin. Identified as from a sauropod dinosaur, possibly a titanosaurid (written communication from Dr. P. Whybrow, Natural History Museum, London; June 9
Journal Article
Published: 01 January 2010
Journal of Paleontology (2010) 84 (1): 137–140.
...) : Journal of Paleontology , 42 , 1 . 96 – 99 . Kear , B. P. , Rich , T. H. , Ali , M. A. , Al-Mufarrih , Y. A. , Matiri , A. H. , Masary , A. M. , and Yousry , A. , 2008 , Late Cretaceous (Campanian-Maastrichtian) marine reptiles from the Adaffa Formation, NW Saudi...
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First thumbnail for: FIRST TRIASSIC LUNGFISH FROM THE ARABIAN PENINSULA
Second thumbnail for: FIRST TRIASSIC LUNGFISH FROM THE ARABIAN PENINSULA
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Fig. 6
Published: 01 December 2012
” northern France [ Leriche, 1929 ], Early Turonian Goulmima [ Cavin, 1999 ], terminal Campanian-Early Maastrichtian of the El Molino Formation, Bolivia [ Gayet, 1991 ], Campanian-Maastrichtian of the Adaffa Formation, Saudi Arabia [ Kear et al. , 2009 ], Maastrichtian of Laño, Spain [ Poyato-Ariza et al
Journal Article
Published: 01 April 2016
Jour. Geol. Soc. India (2016) 87 (4): 469–475.
... et al. (1999) observations the plain of Wadi Ifal occupies most parts of the Midyan basin ( Fig. 1 ). The oldest sedimentary rock unit in the basin is the late Cretaceous Adaffa Formation from Suqah Group (fluviatile in origin), which unconformably overlie the Proterozoic basement rocks. The Suqah...
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Journal Article
Published: 01 December 2012
Bulletin de la Société Géologique de France (2012) 183 (6): 561–572.
...” northern France [ Leriche, 1929 ], Early Turonian Goulmima [ Cavin, 1999 ], terminal Campanian-Early Maastrichtian of the El Molino Formation, Bolivia [ Gayet, 1991 ], Campanian-Maastrichtian of the Adaffa Formation, Saudi Arabia [ Kear et al. , 2009 ], Maastrichtian of Laño, Spain [ Poyato-Ariza et al...
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First thumbnail for: Late Cretaceous (Maastrichtian) ray-finned fishes ...
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Third thumbnail for: Late Cretaceous (Maastrichtian) ray-finned fishes ...
Journal Article
Published: 01 December 2012
Bulletin de la Société Géologique de France (2012) 183 (6): 573–596.
.... The Maastrichtian deposits here consist of marls, limestones with flints, and thin sandy phosphatic levels rich in fish and reptile teeth as well as chelonian shell remains [ Arambourg et al. , 1959 ]. The Late Cretaceous Adaffa Formation (Lower Campanian-Lower Maastrichtian) is composed mainly of sandstone...
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First thumbnail for: Maastrichtian marine reptiles of the Mediterranean...
Second thumbnail for: Maastrichtian marine reptiles of the Mediterranean...
Journal Article
Published: 01 March 2019
Journal of Paleontology (2019) 93 (2): 343–358.
.... 51 , p. 281 – 294 . Kear , B.P. , Rich , T.H. , Ali , M.A. , Al-Mufarrih , Y.A. , Matiri , A.H. , Masary , A.M. , and Attia , Y. , 2008 , Late Cretaceous (Campanian–Maastrichtian) marine reptiles from the Adaffa Formation, NW Saudi Arabia : Geological Magazine...
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First thumbnail for: A dyrosaurid from the Paleocene of Senegal
Second thumbnail for: A dyrosaurid from the Paleocene of Senegal
Third thumbnail for: A dyrosaurid from the Paleocene of Senegal