Venado Formation

Venado Formation
Stratigraphic range: Mid-Late Floian
~475–470 Ma

PreꞒ

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O

S

D

C

P

T

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Venado Formation; Stratigraphic range: Mid-Late Floian; ~475–470 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Type	Geological formation
Unit of	Agua Blanca Group
Underlies	Saldaña Formation
Overlies	Basement
Thickness	up to 670 m (2,200 ft)
Lithology
Primary	Shale
Other	Siltstone, sandstone, pyrite
Location
Coordinates	3°13′21.3″N 74°52′01.4″W
Region	Eastern Ranges, Andes
Country	Colombia
Type section
Named for	Venado River
Named by	Villarroel et al.
Location	Baraya
Year defined	1997
Coordinates	3°13′21.3″N 74°52′01.4″W
Region	Huila
Country	Colombia
Thickness at type section	670 m (2,200 ft)

The Venado Formation (Spanish: Formación Venado, Oir) is a geological formation of the Agua Blanca Group, in the Eastern Ranges of the Colombian Andes, cropping out along the Venado River in northern Huila. The sequence of pyrite containing dark grey micaceous shales interbedded with siltstones and sandstones dates to the Ordovician period; Middle to Late Floian epoch, and has a maximum thickness of 670 metres (2,200 ft) in the type section.

The unit is one of the few Early Paleozoic fossiliferous formations of Colombia; many graptolites of the genus Phyllograptus have been found in the Venado Formation. The graptolites are mostly found in the silty beds and indicative of a fair weather environment on a siliciclastic shallow marine platform at the northern edge of Gondwana. The shallow sea where the Venado Formation was deposited ranged into the deeper cold Iapetus and Rheic Oceans, separating the South American continent of the time from Laurentia, Avalonia and Baltica.

Etymology

The formation was first described by Villarroel et al. in 1997 and named after the Venado River, a left tributary of the Cabrera River.[1][2]

Description

Type locality of the formation in Huila

The Venado Formation is one of few Ordovician formations outcropping in Colombia. The formation, part of the Agua Blanca Group,[3] crops out on both banks of the Venado River in El Totumo, a vereda of the municipality Baraya in the department of Huila.[4] The thickness of the Venado Formation proper at its type section is 670 metres (2,200 ft), put in faulted contact with an overlying 30 metres (98 ft) thin unit and an underlying 50 metres (160 ft) sequence.[1] The series is unconformably overlain by the Jurassic Saldaña Formation.[1][5] The Venado Formation has been correlated to the contemporaneous El Hígado Formation of the Central Ranges in Tarqui.[6][7]

Lithologies

The Venado Formation comprises laminated dark grey micaceaous shales, with intercalating siltstone levels and very fine sandstone beds. Calcareous concretions up to 1 metre (3.3 ft) in diameter are present. The shales frequently contain aggregates of pyrite. The formation is heavily folded and in a faulted contact with the Cretaceous Caballos Formation,[3] at time of definition of the Venado Formation considered part of the Villeta Group.[8]

Depositional environment

The Venado Formation was deposited in a shallow marine environment, on a siliciclastic platform with persistent normal wave action with repetitive storm wave activity.[9] Anoxic conditions of the shallow sea probably led to the deposition of pyrite. The siltstone layers contain fragmented fossils of graptolites and are probably indicative of a fair weather environment and the coarser sediments resulted from episodic and rhythmic storms.[10]

Paleogeography

During the Ordovician, the present-day area of northwestern South America was located in the southern temperate region. The cold[11] Iapetus Ocean to the north of the South American terrane separated the landmass from Laurentia, most of present-day North America. The Rheic Ocean separated South America from the paleocontinents Baltica and Avalonia, that today is part of northeastern North America and northwestern Europe. North of the emerged continent of Gondwana, a shallow sea existed, bordering the Guyana and Brazilian Shields comprising the oldest crustal parts of the current South American continent.[11] During this time in the Ordovician, Gondwana was experiencing an orogeny; the Famatinian orogeny, when the Iapetus Plate was subducting beneath Gondwana.[12]

Fossil content

Fossiliferous formations of the Early Paleozoic are rare in Colombia. Apart from the Venado Formation, El Hígado Formation of the Central Ranges also in Huila, has provided fossils dating to the Ordovician, the Cambrian Duda Formation of the Serranía de Macarena in Meta contains fossils of the trilobite Paradoxides,[13] and the westernmost Ordovician unit in Colombia, La Cristalina Formation in the Central Ranges of eastern Antioquia that provided four species of Didymograptus.[14]

The formation has provided many fossils of graptolites; the most frequently occurring genus is Phyllograptus.[15] Additionally, Villarroel et al. (1997) reported having found Lingulella sp. and Didymograptus cf. D. artus in the formation.[5][9] The latter graptolite genus fossils have been assigned rather to Acrograptus filiformis by Gutiérrez Marco in 2006.[16]

Regional correlations

Stratigraphy of the Llanos Basin and surrounding provinces
Ma	Age	Regional events	Catatumbo	Cordillera	proximal Llanos	distal Llanos	Putumayo	VSM	Environments	Maximum thickness	Petroleum geology	Notes
0.01	Holocene	Holocene volcanism Seismic activity	alluvium								Overburden
1	Pleistocene	Pleistocene volcanism Andean orogeny 3 Glaciations	Guayabo	Soatá Sabana	Necesidad	Guayabo	Gigante Neiva		Alluvial to fluvial (Guayabo)	550 m (1,800 ft) (Guayabo)		[17][18][19][20]
2.6	Pliocene	Pliocene volcanism Andean orogeny 3 GABI		Subachoque			Gigante Neiva
5.3	Messinian	Andean orogeny 3 Foreland		Marichuela			Caimán	Honda				[19][21]
13.5	Langhian	Regional flooding	León	hiatus	Caja	León	Caimán		Lacustrine (León)	400 m (1,300 ft) (León)	Seal	[20][22]
16.2	Burdigalian	Miocene inundations Andean orogeny 2	C1		Carbonera C1		Ospina		Proximal fluvio-deltaic (C1)	850 m (2,790 ft) (Carbonera)	Reservoir	[21][20]
17.3			C2		Carbonera C2				Distal lacustrine-deltaic (C2)		Seal
19			C3		Carbonera C3				Proximal fluvio-deltaic (C3)		Reservoir
21	Early Miocene	Pebas wetlands	C4		Carbonera C4			Barzalosa	Distal fluvio-deltaic (C4)		Seal
23	Late Oligocene	Andean orogeny 1 Foredeep	C5		Carbonera C5		Orito		Proximal fluvio-deltaic (C5)		Reservoir	[18][21]
25	Late Oligocene		C6		Carbonera C6		Orito		Distal fluvio-lacustrine (C6)		Seal
28	Early Oligocene		C7		C7		Pepino	Gualanday	Proximal deltaic-marine (C7)		Reservoir	[18][21][23]
32	Oligo-Eocene		C8	Usme	C8	onlap			Marine-deltaic (C8)		Seal Source	[23]
35	Late Eocene		Mirador	Usme	Mirador				Coastal (Mirador)	240 m (790 ft) (Mirador)	Reservoir	[20][24]
40	Middle Eocene			Regadera				hiatus
45	Middle Eocene
50	Early Eocene		Socha		Los Cuervos				Deltaic (Los Cuervos)	260 m (850 ft) (Los Cuervos)	Seal Source	[20][24]
55	Late Paleocene	PETM 2000 ppm CO₂	Los Cuervos	Bogotá	Los Cuervos			Gualanday	Deltaic (Los Cuervos)	260 m (850 ft) (Los Cuervos)	Seal Source
60	Early Paleocene	SALMA	Barco	Guaduas	Barco		Rumiyaco	Gualanday	Fluvial (Barco)	225 m (738 ft) (Barco)	Reservoir	[17][18][21][20][25]
65	Maastrichtian	KT extinction	Catatumbo	Guadalupe				Monserrate	Deltaic-fluvial (Guadalupe)	750 m (2,460 ft) (Guadalupe)	Reservoir	[17][20]
72	Campanian	End of rifting	Colón-Mito Juan					Monserrate				[20][26]
83	Santonian						Villeta/Güagüaquí
86	Coniacian
89	Turonian	Cenomanian-Turonian anoxic event	La Luna	Chipaque	Gachetá	hiatus			Restricted marine (all)	500 m (1,600 ft) (Gachetá)	Source	[17][20][27]
93	Cenomanian	Rift 2		Chipaque	Gachetá				Restricted marine (all)	500 m (1,600 ft) (Gachetá)	Source
100	Albian			Une	Une		Caballos		Deltaic (Une)	500 m (1,600 ft) (Une)	Reservoir	[21][27]
113	Aptian		Capacho	Fómeque			Motema	Yaví	Open marine (Fómeque)	800 m (2,600 ft) (Fómeque)	Source (Fóm)	[18][20][28]
125	Barremian	High biodiversity	Aguardiente	Paja					Shallow to open marine (Paja)	940 m (3,080 ft) (Paja)	Reservoir	[17]
129	Hauterivian	Rift 1	Tibú- Mercedes	Las Juntas	hiatus				Deltaic (Las Juntas)	910 m (2,990 ft) (Las Juntas)	Reservoir (LJun)	[17]
133	Valanginian		Río Negro	Cáqueza Macanal Rosablanca					Restricted marine (Macanal)	2,935 m (9,629 ft) (Macanal)	Source (Mac)	[18][29]
140	Berriasian		Girón	Cáqueza Macanal Rosablanca					Restricted marine (Macanal)	2,935 m (9,629 ft) (Macanal)	Source (Mac)
145	Tithonian	Break-up of Pangea	Jordán	Arcabuco	Buenavista Batá		Saldaña		Alluvial, fluvial (Buenavista)	110 m (360 ft) (Buenavista)	"Jurassic"	[21][30]
150	Early-Mid Jurassic	Passive margin 2	La Quinta	Montebel Noreán	hiatus		Saldaña		Coastal tuff (La Quinta)	100 m (330 ft) (La Quinta)		[31]
201	Late Triassic	Passive margin 2	Mucuchachi	Montebel Noreán			Payandé					[21]
235	Early Triassic	Pangea		hiatus							"Paleozoic"
250	Permian	Pangea
300	Late Carboniferous	Famatinian orogeny						Cerro Neiva ()				[32]
340	Early Carboniferous	Fossil fish Romer's gap		Cuche (355-385)	Farallones ()			Cerro Neiva ()	Deltaic, estuarine (Cuche)	900 m (3,000 ft) (Cuche)
360	Late Devonian	Passive margin 1	Río Cachirí (360-419)	Cuche (355-385)	Farallones ()			Ambicá ()	Alluvial-fluvial-reef (Farallones)	2,400 m (7,900 ft) (Farallones)		[29][33][34][35][36]
390	Early Devonian	High biodiversity	Floresta (387-400) El Tíbet					Ambicá ()	Shallow marine (Floresta)	600 m (2,000 ft) (Floresta)
410	Late Silurian	Silurian mystery	Floresta (387-400) El Tíbet
425	Early Silurian	Silurian mystery	hiatus
440	Late Ordovician	Rich fauna in Bolivia	San Pedro (450-490)		Duda ()
470	Early Ordovician	First fossils	San Pedro (450-490)	Busbanzá (>470±22) Chuscales Otengá	Guape ()		Río Nevado ()	Hígado () Agua Blanca Venado (470-475)				[37][38][39]
488	Late Cambrian	Regional intrusions	Chicamocha (490-515)	Quetame ()	Ariarí ()		SJ del Guaviare (490-590)	San Isidro ()				[40][41]
515	Early Cambrian	Cambrian explosion		Quetame ()				San Isidro ()				[39][42]
542	Ediacaran	Break-up of Rodinia		pre-Quetame		post-Parguaza		El Barro ()	Yellow: allochthonous basement (Chibcha Terrane) Green: autochthonous basement (Río Negro-Juruena Province)		Basement	[43][44]
600	Neoproterozoic	Cariri Velhos orogeny	Bucaramanga (600-1400)				pre-Guaviare					[40]
800	Neoproterozoic	Snowball Earth										[45]
1000	Mesoproterozoic	Sunsás orogeny			Ariarí (1000)			La Urraca (1030-1100)				[46][47][48][49]
1300		Rondônia-Juruá orogeny			pre-Ariarí	Parguaza (1300-1400)		Garzón (1180-1550)				[50]
1400			pre-Bucaramanga					Garzón (1180-1550)				[51]
1600	Paleoproterozoic					Maimachi (1500-1700)		pre-Garzón				[52]
1800		Tapajós orogeny				Mitú (1800)						[50][52]
1950		Transamazonic orogeny				pre-Mitú						[50]
2200		Columbia
2530	Archean	Carajas-Imataca orogeny										[50]
3100	Archean	Kenorland
Sources

Legend

group
important formation
fossiliferous formation
minor formation
(age in Ma)
proximal Llanos (Medina)[note 1]
distal Llanos (Saltarin 1A well)[note 2]

Notes

based on Duarte et al. (2019)[53], García González et al. (2009),[54] and geological report of Villavicencio[55]
based on Duarte et al. (2019)[53] and the hydrocarbon potential evaluation performed by the UIS and ANH in 2009[56]

References

Villarroel et al., 1997, p.42
Moreno Sánchez, 2008, p.10
Plancha 303, 2002
Moreno Sánchez, 2008, p.11
Moreno Sánchez, 2008, p.13
Moreno Sánchez, 2008, p.9
Borrero et al., 2007, p.44
Villarroel et al., 1997, p.43
Villarroel et al., 1997, p.46
Villarroel et al., 1997, p.47
Moreno Sánchez, 2008, p.14
Chernicoff et al., 2010, p.679
Toro Toro et al., 2014, p.16
González, 2001, p.49
Moreno Sánchez, 2008, p.12
Moreno Sánchez, 2008, p.16
García González et al., 2009, p.27
García González et al., 2009, p.50
García González et al., 2009, p.85
Barrero et al., 2007, p.60
Barrero et al., 2007, p.58
Plancha 111, 2001, p.29
Plancha 177, 2015, p.39
Plancha 111, 2001, p.26
Plancha 111, 2001, p.24
Plancha 111, 2001, p.23
Pulido & Gómez, 2001, p.32
Pulido & Gómez, 2001, p.30
Pulido & Gómez, 2001, pp.21-26
Pulido & Gómez, 2001, p.28
Correa Martínez et al., 2019, p.49
Plancha 303, 2002, p.27
Terraza et al., 2008, p.22
Plancha 229, 2015, pp.46-55
Plancha 303, 2002, p.26
Moreno Sánchez et al., 2009, p.53
Mantilla Figueroa et al., 2015, p.43
Manosalva Sánchez et al., 2017, p.84
Plancha 303, 2002, p.24
Mantilla Figueroa et al., 2015, p.42
Arango Mejía et al., 2012, p.25
Plancha 350, 2011, p.49
Pulido & Gómez, 2001, pp.17-21
Plancha 111, 2001, p.13
Plancha 303, 2002, p.23
Plancha 348, 2015, p.38
Planchas 367-414, 2003, p.35
Toro Toro et al., 2014, p.22
Plancha 303, 2002, p.21
Bonilla et al., 2016, p.19
Gómez Tapias et al., 2015, p.209
Bonilla et al., 2016, p.22
Duarte et al., 2019
García González et al., 2009
Pulido & Gómez, 2001
García González et al., 2009, p.60

Bibliography

Borrero, C.; G.N. Sarmiento; C. Gómez González, and J.C. Gutiérrez Marco. 2007. Los Conodontos de la Formación El Hígado y su contribución al conocimiento del metamorfismo y la paleogeografía del Ordovícico en la Cordillera Central Colombiana. Boletín de Geología 29. 39–46. Accessed 2019-03-07.
Chernicoff, Carlos J.; Eduardo O. Zappettini; João O.S. Santos; Shelley Allchurch, and Neal J. McNaughton. 2010. The southern segment of the Famatinian magmatic arc, La Pampa Province, Argentina. Gondwana Research 17. 662–675. Accessed 2019-03-07.
González, Humberto. 2001. Mapa Geológico del Departamento de Antioquia - 1:400,000 - Memoria explicativa, 1–120. INGEOMINAS.
Moreno Sánchez, Mario; Arley de Jesus Gómez Cruz, and Hardany Castillo González. 2008. Graptolitos del Ordovícico y geología de los afloramientos del Río Venado (norte del Departamento del Huila). Boletín de Geología 30. 9–19. Accessed 2019-03-07.
Toro Toro, Luz Mary; Mario Moreno Sánchez, and Arley Gómez Cruz. 2014. Metagabro del Ariarí, plutonismo MORB, Cordillera Oriental de Colombia. Boletín de Geología 36. _. Accessed 2019-03-07.
Villarroel A., C.; C. Macia S., and J. Brieva B. 1997. Formación Venado, nueva unidad litoestratigráfica del Ordovícico colombiano. Geología Colombiana 22. 41–49. Accessed 2019-03-07.

Maps

Acosta, Jorge; Pablo Caro; Jaime Fuquen, and José Osorno. 2002. Plancha 303 - Colombia - 1:100,000, 1. INGEOMINAS.

External links

(in Spanish) Hallados en Colombia fósiles de hace 488 millones de años

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[56] sed on Duarte et al. (2019)[53], García González et al. (2009),[54] and geological report of Villavicencio[55]

[58] sed on Duarte et al. (2019)[53] and the hydrocarbon potential evaluation performed by the UIS and ANH in 2009[56]

[Villarroel1997_p42-1] Villarroel et al., 1997, p.42

[Moreno2008_p10-2] Moreno Sánchez, 2008, p.10

[Plancha303-3] Plancha 303, 2002

[Moreno2008_p11-4] Moreno Sánchez, 2008, p.11

[Moreno2008_p13-5] Moreno Sánchez, 2008, p.13

[Moreno2008_p9-6] Moreno Sánchez, 2008, p.9

[Borrero2007_p44-7] Borrero et al., 2007, p.44

[Villarroel1997_p43-8] Villarroel et al., 1997, p.43

[Villarroel1997_p46-9] Villarroel et al., 1997, p.46

[Villarroel1997_p47-10] Villarroel et al., 1997, p.47

[Moreno2008_p14-11] Moreno Sánchez, 2008, p.14

[Chernicoff2010_p679-12] Chernicoff et al., 2010, p.679

[ToroToro2014_p16-13] Toro Toro et al., 2014, p.16

[Gonzalez2001_p49-14] González, 2001, p.49

[Moreno2008_p12-15] Moreno Sánchez, 2008, p.12

[Moreno2008_p16-16] Moreno Sánchez, 2008, p.16

[UISANH2009_p27-17] García González et al., 2009, p.27

[UISANH2009_p50-18] García González et al., 2009, p.50

[UISANH2009_p85-19] García González et al., 2009, p.85

[ANH2007_p60-20] Barrero et al., 2007, p.60

[ANH2007_p58-21] Barrero et al., 2007, p.58

[Plancha111_p29-22] Plancha 111, 2001, p.29

[Plancha177_p39-23] Plancha 177, 2015, p.39

[Plancha111_p26-24] Plancha 111, 2001, p.26

[Plancha111_p24-25] Plancha 111, 2001, p.24

[Plancha111_p23-26] Plancha 111, 2001, p.23

[Pulido2001_p32-27] Pulido & Gómez, 2001, p.32

[Pulido2001_p30-28] Pulido & Gómez, 2001, p.30

[Pulido2001_pp21_26-29] Pulido & Gómez, 2001, pp.21-26

[Pulido2001_p28-30] Pulido & Gómez, 2001, p.28

[Correa2019_p49-31] Correa Martínez et al., 2019, p.49

[Plancha303_p27-32] Plancha 303, 2002, p.27

[Terraza2008_p22-33] Terraza et al., 2008, p.22

[Plancha229_pp46_55-34] Plancha 229, 2015, pp.46-55

[Plancha303_p26-35] Plancha 303, 2002, p.26

[Moreno2009_p53-36] Moreno Sánchez et al., 2009, p.53

[Figueroa2015_p43-37] Mantilla Figueroa et al., 2015, p.43

[Manosalva2017_p84-38] Manosalva Sánchez et al., 2017, p.84

[Plancha303_p24-39] Plancha 303, 2002, p.24

[Figueroa2015_p42-40] Mantilla Figueroa et al., 2015, p.42

[Arango2012_p25-41] Arango Mejía et al., 2012, p.25

[Plancha350_p49-42] Plancha 350, 2011, p.49

[Pulido2001_pp17_21-43] Pulido & Gómez, 2001, pp.17-21

[Plancha111_p13-44] Plancha 111, 2001, p.13

[Plancha303_p23-45] Plancha 303, 2002, p.23

[Plancha348_p38-46] Plancha 348, 2015, p.38

[Plancha367_414_p35-47] Planchas 367-414, 2003, p.35

[Toro2014_p22-48] Toro Toro et al., 2014, p.22

[Plancha303_p21-49] Plancha 303, 2002, p.21

[Bonilla2016_p19-50] Bonilla et al., 2016, p.19

[GeoMap2015_p209-51] Gómez Tapias et al., 2015, p.209

[Bonilla2016_p22-52] Bonilla et al., 2016, p.22

[Duarte2019-53] Duarte et al., 2019

[UISANH2009-54] García González et al., 2009

[Pulido2001-55] Pulido & Gómez, 2001

[UISANH2009_p60-57] García González et al., 2009, p.60