Maevarano Formation

The Maevarano Formation is well exposed in the Mahajanga Basin, in particular near the village of Berivotra near the northwestern coast of the island where its outcrops have been heavily dissected by erosion. At the time it was being deposited, its latitude was between 30°S and 25°S as Madagascar drifted northward after splitting from India about 88 million years ago. It is composed of three smaller units or members. The lowest is the Masorobe Member, which is usually reddish and is at least {{convert|80|m|ft}}. Its rocks are mostly poorly sorted coarse-grained sandstones with some finer-grained beds. It is separated by an erosional disconformity from the next member, the Anembalemba Member. The lower portion of the Anembalemba Member is fine to coarse clay-rich sandstone, whitish or light grey in color, with cross-bedding. The upper portion of this member is made of poorly sorted clay-rich sandstone, light olive-grey in color, that lacks cross-bedding. Most vertebrate fossils come from the Anembalemba Member, especially from the upper portion. The Miadana Member, the third and uppermost member, is not always present, and is up to {{convert|25|m|ft}} in some places. Elsewhere, it is replaced by the marine Berivotra Formation. The Miadana Member is made up of claystone, siltstone, and sandstone, lacks cross-bedding, and has several colors of rock. The Maevarano Formation as a whole is underlain by the Marovoay beds and capped by the Berivotra Formation.Rogers et al., 2007

The age of the Maevarano Formation has been debated; the Berivotra Formation, which is partially contemporaneous with the upper portions of the formation, shows that at least the upper part of the Maevarano is Maastrichtian in age. There is no evidence that it is Campanian, despite previous reports to that effect.Weishampel et al., 2004 The Berivotra Formation appears to include near its top a magnetic reversal, interpreted as the shift from Chron 30N to Chron 29R, which occurred approximately 65.8 million years ago (about 300,000 years before the Cretaceous–Paleogene boundary and associated Cretaceous–Paleogene extinction event. This suggests that Maevarano organisms also lived shortly before (geologically speaking) the extinction event.

The Maevarano Formation was first explored by French military physician Dr. Félix Salètes and his staff officer Landillon in 1895, and fossils and geologic data were sent to paleontologist Charles Depéret.Krause et al., 2007b He briefly described the formation and named two dinosaurs from the remains (Titanosaurus madagascariensis and Megalosaurus crenatissimus, now Majungasaurus).Depéret, 1896 Similar collections were made throughout the 20th century, yielding mostly fragmentary fossils; one such specimen, a rough partial skull roof, became the holotype of supposed pachycephalosaur (bonehead dinosaur) Majungatholus in 1979.Sues & Taquet, 1979 (This specimen was later shown to be part of the skull ornamentation of a Majungasaurus.) Large-scale expeditions (seven to date), under the banner of the Mahajanga Basin Project, began in 1993. These expeditions, conducted jointly by Stony Brook University and the University of Antananarivo, have greatly expanded knowledge of this formation and the organisms that lived while it was being deposited.

File:Majungasaurus, Masiakasaurus, Rapetosaurus.jpg, Masiakasaurus and Rapetosaurus during the late Cretaceous]]

The Maevarano Formation is interpreted as a low-relief alluvial plain that over time was covered by a marine transgression. Broad, shallow rivers flowed to the northwest from central highlands; evidence for debris flows suggests that the discharges of the rivers varied greatly, with periods of dilute water flow, and periods of rapid erosion dumping sediment into the channels. Paleosols are reddish and include root casts. The paleosols and other sedimentologic evidence indicate well-drained floodplains with abundant vegetation adapted to a relatively dry climate, strongly seasonal (rainy and dry seasons) and at times semiarid (not unlike the present climate of the area).

Animals found in the formation include frogs (including Beelzebufo ampinga),{{cite journal |last=Evans |first=Susan E. |author2=Jones, Marc E. H. |author3=Krause, David W. |year=2008 |title=A giant frog with South American affinities from the Late Cretaceous of Madagascar |journal=Proceedings of the National Academy of Sciences of the United States of America |volume=105 |issue=8 |pages=2951–2956 |doi=10.1073/pnas.0707599105 |pmid=18287076 |pmc=2268566 |bibcode=2008PNAS..105.2951E |doi-access=free }} turtles, snakes, lizards, at least seven species of crocodyliforms (including species of Mahajangasuchus and Miadanasuchus), abelisaurid theropod Majungasaurus, noasaurid Masiakasaurus, two types of titanosaurian sauropods (Rapetosaurus and Vahiny), and at least five species of bird-like dinosaurs, including Rahonavis. The {{convert|6|to|7|m|ft}} long Majungasaurus was likely the apex predator in the terrestrial environment. Crocodyliforms were very diverse and abundant.

{{paleobiota-key-compact}}

Indeterminate Lithostrotia remains formerly attributed to Titanosauridae. Undescribed Lithostrotia form. Indeterminate Enantiornithes remains. A rich avifauna with several undescribed taxa are known, including pengornithid enantiornithes and putative omnivoropterygids.O'Connor and Forster, 2010. A Late Cretaceous (Maastrichtian) avifauna from the Maevarano Formation, Madagascar. Journal of Vertebrate Paleontology. 30(4), 1178-1201.

Mammal remains include an undescribed gondwanathere,Krause et al, 2014 a broken tooth UA 8699, which has been interpreted both as metatherian and as eutherian, a non-gondwanathere multituberculate tooth fragment, a non-gondwanathere multituberculate femur,{{cite journal |last1=Krause |first1=David W. |last2=Hoffmann |first2=Simone |last3=Werning |first3=Sarah |title=First postcranial remains of Multituberculata (Allotheria, Mammalia) from Gondwana |journal=Cretaceous Research |date=December 2017 |volume=80 |pages=91–100 |doi=10.1016/j.cretres.2017.08.009 |bibcode=2017CrRes..80...91K |doi-access=free }} and a yet undescribed mammal known from an articulated skeleton.{{cite journal |last1=Krause |first1=David W. |last2=O'Connor |first2=Patrick M. |last3=Rogers |first3=Kristina Curry |last4=Sampson |first4=Scott D. |last5=Buckley |first5=Gregory A. |last6=Rogers |first6=Raymond R. |title=Late Cretaceous terrestrial vertebrates from Madagascar: Implications for Latin American biogeography |journal=Annals of the Missouri Botanical Garden |date=23 August 2006 |volume=93 |issue=2 |pages=178–208 |doi=10.3417/0026-6493(2006)93[178:LCTVFM]2.0.CO;2 |jstor=40035721 |s2cid=9166607 |url=https://www.biodiversitylibrary.org/part/390696 }} Some taxa are particularly large sized herbivores, exemplifying the diversity of Mesozoic mammals.Krause et al., 2020

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• Lists of fossiliferous stratigraphic units in Africa
• List of fossiliferous stratigraphic units in Madagascar
• Geology of Madagascar

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== References ==

{{Reflist}}

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Category:Geologic formations of Madagascar

Category:Upper Cretaceous Series of Africa

Category:Cretaceous Madagascar

Category:Maastrichtian Stage

Category:Sandstone formations

Category:Shale formations

Category:Alluvial deposits

Category:Deltaic deposits

Category:Fluvial deposits

Category:Lacustrine deposits

Category:Paleontology in Madagascar

Formations