Mata Amarilla Formation

Coordinates: 49°30′S 71°30′W / 49.5°S 71.5°W / -49.5; -71.5
Source: Wikipedia, the free encyclopedia.
Mata Amarilla Formation
Ma
Approximate paleocoordinates
56°30′S 48°48′W / 56.5°S 48.8°W / -56.5; -48.8
RegionSanta Cruz Province
CountryArgentina
ExtentAustral Basin
Stratigraphic column
Stratigraphic column

The Mata Amarilla Formation is a

Pari Aike Formation
.

The Mata Amarilla Formation has provided many fossil vertebrates, among which dinosaurs, fish and turtles, as well as fossil insects, flora and molluscs.

Age

Paleogeography of the Late Cretaceous (90 Ma) with known distribution of Arcellites disciformis indicated

The middle section of the Mata Amarilla Formation has widely been regarded as Maastrichtian in age, but recent dating of a lava tuff layer shows that it dates back to 96.2 ± 0.7 Ma, during the Cenomanian.[1]

Description

The Austral (or Magallanes) Basin, is located on the southwestern end of the South American Plate and it is bordered to the south by the Scotia Plate covering an area of approximately 230.000 square kilometres (88.803 sq mi). In the studied area, the Austral Basin underwent three main tectonic stages: (i) a rift stage; (ii) a thermal subsidence stage; and (iii) a foreland stage.

The rifting stage is related to the break-up of Gondwana, grabens and half-grabens were formed and filled with volcaniclastic and volcanic rocks intercalated with epiclastic sediments of the El Quemado and Tobífera Formations.[2]

Subsequently, the

transgressive quartzose sandstone of the Springhill Formation, and the black mudstone and marl of the Río Mayer Formation. Towards the end of this stage, the Piedra Clavada Formation
was deposited, representing a large passive-margin delta system.

The foreland stage, in response to the regional change from extensive to compressive regime, resulted in the deposition of the continental Mata Amarilla Formation. This unit is mainly composed of grey and blackish

claystone, alternating with whitish and yellowish-grey fine to medium grained sandstone
. Varela (2014) recognized three informal sections (lower, middle, and upper) on the bases of sedimentological and sequence stratigraphic analysis. The lower section consists of fine-grained intervals with paleosols interbedded with laminated shale and coquina, representing coastal plain and lagoon paleoenvironments.

The middle section comprises

lacustrine
deposits. The upper section is dominated by fine-grained deposits, related to distal fluvial channels.

Paleosol features and paleosol-derived climatic proxies suggest a subtropical temperate-warm, at 12 ± 2.1 °C (53.6 ± 3.8 °F) and humid, with 1,404 ± 108 millimetres (55.3 ± 4.3 in)/yr, climate with marked rainfall seasonality during the deposition of this unit (Varela et al. 2012b; 2018), in accordance with previous paleobotanical interpretations.[3]

Fossil content

Dinosaurs

Dinosaurs
Genus Species Location Stratigraphic position Material Notes Images
Clasmodosaurus C. spatula Middle Section
Loncosaurus L. argentinus Middle Section

References

  1. ^ Varela et al., 2012
  2. ^ Santamarina et al., 2018, p.608
  3. ^ Santamarina et al., 2018, p.609
  4. ^
    S2CID 245549530
    .
  5. ^ Cerro Waring at Fossilworks.org
  6. ^ Santamarina et al., 2018, p.610

Bibliography

Further reading