The Paja Formation (, 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 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 is famous for its vertebrate fossils and is the richest Mesozoic fossiliferous formation of Colombia. Several marine reptile fossils of plesiosaurs, pliosaurs, ichthyosaurs 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.
Description The Paja Formation was first described by O.C. Wheeler, according to Morales (1958),Morales, 1958 and named after Quebrada La Paja, a tributary of the Sogamoso River. The type section is exposed on the northern banks of the quebrada at the confluence of the Sogamoso River in Betulia, Santander.Reyes et al., 2006, p.33Plancha 120, 2010
The formation is divided into the Lutitas Negras Inferiores, Arcillolitas Abigarradas and Arcillolitas con Nódulos Huecos Members, and stretches across from northeast to southwest. The Paja Formation overlies the Ritoque and Rosablanca Formations and is overlain by the Simití and Tablazo Formations and dates from the Hauterivian to Late Aptian.
Outcrops
The type section of the Paja Formation is found at the banks of Quebrada La Paja in Betulia, Santander, where the formation has a thickness of .Patarroyo & Moreno, 1997, p.30 Outcrops of the formation extend from Simití in the north, close to the border of Santander and Bolívar, where the formation is offset by the Simití Fault,Plancha 85, 2006 to the Pauna Anticlinal in San Pablo de Borbur, where the formation is thrusted over the Ritoque Formation in the south.Plancha 190, 1998 In the southern extension of the exposures, the formation crops out in the north of Tununguá, near the Ibacapí Fault.Reyes et al., 2006, p.32
Santander In the Middle Magdalena Valley, south of Barrancabermeja, the Paja Formation in the subsurface is offset by the Casabe, Infantas and Arruga Faults.Plancha 119, 2008 In the northeastern extent, in Río Negro, near the border with Norte de Santander, the formation is found in the subsurface, offset by the Lebríja Fault.Plancha 97, 2009 The town center of Zapatoca rests on the formation in the synclinal named after the village. The Paja Formation also crops out in the northwestern part of the Middle Magdalena Valley, east of San Pablo, Bolívar, where in the formation underlies the Simití Formation and is offset in the subsurface by the Pozo Azul and Caña Braval Faults.Plancha 96, 2006 South of there, the Paja Formation is offset by the La Corcovada and El Guineal Faults,Plancha 149, 2008 and the regional La Salina Fault.Plancha 134, 2008 Near the eponymous town, the formation is offset by the Landazurí Fault.Plancha 150, 2008
West of Barichara, the formation underlies the corregimiento and is found in the hills bordering both sides of the Suárez River. In this area, the Paja Formation is offset by the Suárez Fault.Royero & Clavijo, 2001, p.53 Surrounding Jordán, Santander, the formation crops out on both sides of the Chicamocha River in the Chicamocha Canyon. The touristic town San Gil rests on the formation and the Fonce River cuts into it. East of the town center, the formation is offset by the Curití and Ocamonte Faults.Plancha 135, 2009 The urban centers of Oiba, San Benito, Encino, Ocamonte and Charalá are built on top of the Paja Formation. In this area, the formation is offset by the Confines and Encino Faults.Plancha 151, 2009 Further to the south, the towns of Vélez, Guavatá and Jesús María rest on the formation. West of the latter, the Paja Formation is put in a reverse faulted contact with the Cumbre Formation.Plancha 170, 2009 The El Carmen Fault puts the Paja Formation in contact with the Jurassic Girón Formation.
Boyacá
In northeastern Boyacá, the formation underlies the urban center of Moniquirá (not to be confused with Monquirá, a vereda of nearby Villa de Leyva) and is crossed by the Moniquirá River. West of Arcabuco in the Villa de Leyva Synclinal, the formation is cut by the Arcabuco River.Plancha 171, 2009 In the vicinity of Pauna and San Pablo de Borbur, the formation crops out in an extensive area. Here, the Paja Formation is offset by the Río Minero and Pedro Gómez Faults and occurs in the footwall of the La Venta Fault.Reyes et al., 2006, p.83 North of Lake Fúquene, the town centers of Tinjacá and Sutamarchán are built on top of the Paja Formation. In this area, the formation extends into the northern part of Cundinamarca, where the urban centers of Yacopí and La Palma rest on the formation.Plancha 189, 2005
Villa de Leyva Surrounding the touristic town of Villa de Leyva, the formation crops out in the hills in a microclimatic location, known as the La Candelaria Desert (), stretching across Villa de Leyva, Santa Sofía and Sáchica.Plancha 191, 1998 Along the highway Tunja-Villa de Leyva, the formation is heavily folded and faulted along a stretch of .Moreno & Hincapié, 2010, p.44 In the vicinity of Villa de Leyva, the formation has provided many fossils of marine reptiles, as well as the dinosaur Padillasaurus.
Stratigraphy
The Paja Formation overlies the Ritoque and Rosablanca Formations and is concordantly overlain by the San Gil Group and Tablazo Formations in the eastern extent,Royero & Clavijo, 2001, p.31 and the Simití Formation in the northwestern Middle Magdalena Valley. In the Western emerald belt, the contact with the Rosablanca Formation is concordant and abrupt.Reyes et al., 2006, p.26 The total thickness of the formation varies across its extent, but can reach up to .Moreno & Hincapié, 2010, p.26
Members The Paja Formation is subdivided into three members, from oldest to youngest:
Lutitas Negras Inferiores (Lower Black Shales) – a sequence of of black shales and sandy shales with a segment containing calcareous nodules. The age of this member is estimated at late Hauterivian, based on ammonites analyzed by Fernando Etayo.Moreno & Hincapié, 2010, p.25 Arcillolitas Abigarradas (Mottled Claystones) – a series of multicolored claystones with abundant calcareous fossiliferous nodules, reaching a thickness of . In the upper of this member, intercalations of gypsum occur. The age of the middle member of the Paja Formation is estimated at early Barremian to late Aptian on the basis of ammonites described by Fernando Etayo. Arcillolitas con Nódulos Huecos (Claystones with Hollow Nodules) – the upper member of the formation of approximately thick consists of yellowish and grey claystones containing hollow nodules. Ammonite analysis has led to an estimated late Aptian age for the member.
In the northern part of the Middle Magdalena Valley, the Paja Formation comprises dark grey to blueish shales, intercalated with grey to yellowish fine-grained sandstones and fossiliferous limestones, locally with a sandy component.Sarmiento et al., 2015, p.65 Bürgl in 1954 reported beds of tuff in the Paja Formation near Villa de Leyva.Sarmiento Rojas, 2002, p.56 Thin section analysis of samples of the Paja Formation has provided insight in the micritic components of the sediments, where three microfacies were recognized; biomicritic wackestones, foraminiferous packstones and sandy biomicritic floatstones containing fragments of echinoderms, bivalves, crinoids and gastropods cemented by hematite.Espinel & Hurtado, 2010, p.70
The Paja Formation correlates with the Tibasosa Formation to the east on the northern Altiplano Cundiboyacense in Boyacá and with the El Peñón Formation pertaining to the Villeta Group to the south in the Eastern Ranges. The formation is laterally equivalent with the black shales of the Fómeque Formation in the eastern part of the Eastern Ranges and the sandstones of Las Juntas Formation in the Sierra Nevada del Cocuy.Villamil, 2012, p.168 In the Middle Magdalena Valley to the west, the formation partly overlies and partly is laterally equivalent to the limestones of the Rosablanca Formation. The Paja Formation is diachronous with the Ritoque and Rosablanca Formations. To the northeast of the extent of the formation, it correlates with the upper part of the Río Negro Formation,Royero & Clavijo, 2001, p.29 and the lowermost Tibú-Mercedes Formation of the Catatumbo Basin.Royero & Clavijo, 2001, p.32
Paleogeography
During deposition of the Paja Formation, the paleo coastline was oriented west–east.Rivera et al., 2018, p.30
From the late Aptian to early Albian, the area was covered by an extensive carbonate platform, in the extent of the Paja Formation represented by the San Gil Group, Tablazo Formation and Villeta Group.Villamil, 2012, p.164
Depositional environment The thin section analysis led to the interpretation of a shoreface to lower shoreface environment,Gaona Narváez et al., 2013 in the internal parts of a carbonate platform,Espinel & Hurtado, 2010, p.73Espinel & Hurtado, 2010, p.89 where transgressions and regressions caused the variations in grain sizes and lithologies.Galvis & Valencia, 2009, p.79 The Barremian to Aptian sequence shows evidence of an overall relative sea level fall with open marine sedimentation in the lowest member and tidal deposits in the upper part of the formation.Galvis & Valencia, 2009, p.81
One of the longest anoxic intervals of geologic history occurred during the Cretaceous, from about 125 to 80 Ma (early Aptian to early Campanian). During this Oceanic Anoxic Event, there were two spikes, the Selli event, dating to the early Aptian (approximately 120 Ma) was active during deposition of the black shales of the Paja Formation.Moreno & Hincapié, 2010, p.48 The formation contains three spikes of δ13C, with values above 1.5‰, in the lower, middle to upper and upper Paja Formation.Moreno & Hincapié, 2010, p.63 These spikes indicate a global change in the carbon cycle and the preservation of organic matter due to poor oxygenation of sea waters. The cause of these elevated δ13C levels may have been a global increase in volcanic activity.Moreno & Hincapié, 2010, p.64
Mining and petroleum geology