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Paja Formation information


Paja Formation
Stratigraphic range: Late Hauterivian-Late Aptian
~130–113 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
Desmatochelys padillai from the Paja Formation
TypeGeological formation
Sub-unitsLutitas Negras Inferiores, Arcillolitas Abigarradas & Arcillolitas con Nódulos Huecos Members
UnderliesSan Gil Group, Simití & Tablazo Formations
OverliesRitoque & Rosablanca Formations
Area450 km (280 mi)
Thicknessup to 940 m (3,080 ft)
Lithology
PrimaryBlack shale, claystone, sandstone and limestone concretions
OtherGypsum, chalcopyrite, galena, malachite, pyrite, sphalerite
Location
Coordinates5°30′N 73°30′W / 5.5°N 73.5°W / 5.5; -73.5
Approximate paleocoordinates3°42′N 42°12′W / 3.7°N 42.2°W / 3.7; -42.2
RegionBolívar, Boyacá, Cundinamarca & Santander
CountryPaja Formation Colombia
ExtentAltiplano Cundiboyacense
Eastern Ranges, Andes
Middle Magdalena Valley
Type section
Named forQuebrada La Paja
Named byWheeler
Year defined1929?
Coordinates7°01′33.4″N 73°19′27.8″W / 7.025944°N 73.324389°W / 7.025944; -73.324389
RegionBetulia, Santander
Thickness at type section625 m (2,051 ft)

Outcrops of the Paja Formation near Villa de Leyva

The Paja Formation (Spanish: Formación Paja, K1p, Kip, Kimp, b3b6p) is an Early Cretaceous geologic formation of central Colombia. The formation extends across the northern part of the Altiplano Cundiboyacense, the Western Colombian emerald belt and surrounding areas of the Eastern Ranges of the Colombian Andes. In the subsurface, the formation is found in the Middle Magdalena Valley to the west. The Paja Formation stretches across four departments, from north to south the southernmost Bolívar Department, in Santander, Boyacá and the northern part of Cundinamarca. Well known fossiliferous outcrops of the formation occur near Villa de Leyva, also written as Villa de Leiva, and neighboring Sáchica.

The formation was named after Quebrada La Paja in Betulia, Santander, and stretches across 450 kilometres (280 mi) from northeast to southwest. The Paja Formation overlies the Ritoque and Rosablanca Formations and is overlain by the San Gil Group and the Simití and Tablazo Formations and dates from the late Hauterivian to late Aptian. The Paja Formation comprises mudstones, shales and nodules of sandstones and limestones, deposited in an anoxic environment, in the warm and shallow sea that covered large parts of the present Colombian territory during the Cretaceous.

Initially considered to host Colombian emeralds, the emerald-bearing part was redefined as a separate formation; the Muzo Formation. The Paja Formation Lagerstätte[1] is famous for its vertebrate fossils and is the richest Mesozoic fossiliferous formation of Colombia. Several marine reptile fossils of plesiosaurs, pliosaurs, ichthyosauras and turtles have been described from the formation and it hosts the only dinosaur fossils described in the country to date; Padillasaurus. The formation also has provided many ammonites, fossil flora, decapods and the fossil shark Protolamna ricaurtei.

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separate genus. The site where Monquirasaurus was discovered is the Paja Formation, that was once an environment containing a vast diversity of marine...

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Cretoxyrhina

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Kronosaurus

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specimen, nicknamed "El Fósil" and dating from the Upper Aptian of the Paja Formation, was first provisionally referred to the genus Kronosaurus two years...

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which the same formation is exposed. Such sites may have separate entries if they are considered to be more notable than the formation as a whole. In...

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ecological network of the marine Mesozoic fauna from the Lower Cretaceous Paja Formation (Colombia), who report that the largest marine reptile predators from...

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