Galula Formation

Geological formation in Tanzania From Wikipedia, the free encyclopedia

The Galula Formation is a geological formation located south of Lake Rukwa in Tanzania, part of the Red Sandstone Group of the Rukwa Rift Basin. Along with the unconformably overlying Oligocene Nsungwe Formation. It is divided into two members, the lower Mtuka Member and the upper Namba Member.[1]

Unit ofRed Sandstone Group
Sub-unitsMtuka Member, Namba Member
UnderliesUnconformity with Nsungwe Formation
Quick facts Type, Unit of ...
Galula Formation
Stratigraphic range: Aptian-Campanian
~120–75 Ma
TypeGeological formation
Unit ofRed Sandstone Group
Sub-unitsMtuka Member, Namba Member
UnderliesUnconformity with Nsungwe Formation
OverliesUnconformity with Karoo Supergroup or basement
Thickness600–3,000 m (2,000–9,800 ft)
Lithology
PrimarySandstone
OtherConglomerate, mudstone
Location
Coordinates7.1°S 31.2°E / -7.1; 31.2
Approximate paleocoordinates28.8°S 16.5°E / -28.8; 16.5
RegionRukwa Region, Songwe Region
CountryTanzania
ExtentAfrican Great Lakes, Rukwa Rift Basin
Type section
Named forGalula
Named byRoberts et al.
LocationGalula Coalfields
Year defined2010
Coordinates8°40′55.6″S 32°53′33.5″E
Thickness at type section520 m (1,710 ft)
Galula Formation is located in Tanzania
Galula Formation
Galula Formation (Tanzania)
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The age of the deposit is poorly constrained, with the Mtuka Member likely being Aptian to Cenomanian in age, while the Namba Member being Cenomanian to Campanian in age based on Geomagnetic reversals.[2] It is correlated with the Dinosaur Beds of Malawi.

The formation is fossiliferous, with Dinosaurs and Crocodyliformes being known from the formation.

Geology

Lithology

The Lithology of the formation is a sequence of red, pink, purple and occasionally white colored sandstones, conglomerates and mudstones. The Mtuka member is 160–180 m thick in the type section, and is typified by coarser sandstone, a higher frequency of conglomerates, higher proportions of extraformational clasts, thicker and a greater frequency of overbank siltstone and mudstone lenses and a higher proportion of paleosols. While the Namba member is between 340–360 m in the type section, and is less variable in facies, predominated by very fine-to medium-grained sandstones with less overbank mudstone and siltstone lenses.[1]

Vertebrate paleofauna

Fish

More information Fish of the, Genus ...
Fish of the Galula Formation
GenusSpeciesLocality Stratigraphic positionAbundanceNotesImages
Lupaceradotus L. useviaensis RRBP 2004-06-30 Lungfish
Ceratodontidae Indeterminate Mtuka Member Lungfish
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Crocodyliformes

More information Crocodyliformes of the, Genus ...
Crocodyliformes of the Galula Formation
GenusSpeciesLocality Stratigraphic positionAbundanceNotesImages
Pakasuchus[3] P. kapilimai RRBP 2007-04[3] Namba Member[3] [Two] skulls and an articulated skeleton.[3] A notosuchian crocodyliform with mammal-like teeth.[3]
Rukwasuchus[4] R. yajabalijekundu Namba 2[4] Middle Namba member[4] A partial skull and isolated teeth.[4] A notosuchian crocodyliform, and the only known sub-Saharan peirosaurid from Africa.[4]
Notosuchia[5] Indeterminate Namba Member[5]
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Dinosaurs

More information Dinosaurs of the, Genus ...
Dinosaurs of the Galula Formation
GenusSpeciesLocality Stratigraphic positionAbundanceNotesImages
Mnyamawamtuka[6] M. moyowamkia Mtuka Member[6] An anterior cervical vertebral neural arch, cervical vertebral centra, partial dorsal vertebrae, sacral neural arch, partial sacral centra, sacral ribs, caudal vertebral neural arches, centra, chevrons, numerous dorsal rib fragments, scapula, sternal plate, humeri, partial ulna, metacarpal I, metacarpal III, partial ischium, partial pubis, partial femora, tibiae, fibula, metatarsal I, metatarsal II, metatarsal III, metatarsal IV, metatarsal V, pedal phalanges, ungual, and numerous unidentifiable fragments.[6] A basal lithostrotian titanosaur with heart-shaped caudal vertebrae.[6]
Rukwatitan[7] R. bisepultus Locality RRBP 2007-02 (Namba 2)[6] Middle Namba member[6] Posterior cervical vertebrae, partial anterior dorsal vertebral neural arch, anterior caudal vertebrae, middle caudal vertebrae, chevrons, multiple partial dorsal ribs, distal scapula, partial coracoids, humerus, partial ulna, ilium, and proximal pubis.[6] A basal lithostrotian titanosaur.[6]
Shingopana[5] S. songwensis TZ-07[6] Namba Member[5] An angular, partial anterior cervical vertebra, partial middle-to-posterior cervical vertebrae, partial cervical ribs, partial dorsal ribs, humerus, pubis, and many incomplete and/or unidentifiable fragments pertaining to the axial skeleton.[6] A lithostrotian titanosaur.[6]
Theropoda[8] Indeterminate Mtuka and Namba Members[8] A pair of articulated proximal caudal vertebrae, and 11 teeth.[5] An indeterminate theropod.[5]
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Turtles

More information Turtles of the, Genus ...
Turtles of the Galula Formation
GenusSpeciesLocality Stratigraphic positionAbundanceNotesImages
Testudines[5] Indeterminate Mtuka and Namba Members.[5] Plastron and carapace fragments.[5]
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Mammals

More information Mammals of the, Genus ...
Mammals of the Galula Formation
GenusSpeciesLocality Stratigraphic positionAbundanceNotesImages
Galulatherium[9] G. jenkinsi TZ-07 Namba Member Left dentary Probable Gondwanathere[10]
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References

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