PhotosLocation


rio+neuquen+formation Latitude and Longitude:

37°24′S 69°06′W / 37.4°S 69.1°W / -37.4; -69.1
From Wikipedia, the free encyclopedia
(Redirected from Rio Neuquen Formation)
Río Neuquén Subgroup
Stratigraphic range: Late Turonian- Late Coniacian
~91–86  Ma
O
S
D
C
P
T
J
K
N
Type Subgroup
Unit of Neuquén Group
Sub-units Plottier, Sierra Barrosa, Los Bastos & Portezuelo Formations
Underlies Río Colorado Subgroup
Overlies Río Limay Subgroup
ThicknessUp to 155 m (509 ft)
Lithology
Primary Sandstone
Other Claystone, limestone, mudstone
Location
Coordinates 37°24′S 69°06′W / 37.4°S 69.1°W / -37.4; -69.1
Approximate paleocoordinates 42°12′S 49°24′W / 42.2°S 49.4°W / -42.2; -49.4
Region Mendoza, Río Negro & Neuquén Provinces
Country  Argentina
Extent Neuquén Basin
Type section
Named for Neuquén River
Río Neuquén Subgroup is located in Argentina
Río Neuquén Subgroup
Río Neuquén Subgroup (Argentina)

The Río Neuquén Subgroup is a geological subgroup in the Neuquén Basin, Neuquén Province, Argentina, whose strata date back to the Late Cretaceous. The subgroup, formerly defined as a formation, is the middle unit of the Neuquén Group and contains the Plottier, Sierra Barrosa Formation, [1] Los Bastos Formation, [2] and Portezuelo Formations. [3] [4] [5] The subgroup overlies the Río Limay Subgroup and is overlain by the Río Colorado Subgroup. [6] Dinosaur remains are among the fossils that have been recovered from the formation. [7]

Fossil content

Dinosaurs
Genus Species Location Stratigraphic position Material Notes Images
Antarctosaurus [8] A. giganteus [8] "[Two] femora, pubis." [9] Río Neuquén remains previously referred to A. giganteus are now attributed to an indeterminate sauropod. [8]
A. wichmannianus [8]
Megaraptor [8] M. namunhuaiquii [8] "Partial forelimb, manus, and pes." [10]
Patagonykus [8] P. puertai [8] "Partial postcranial skeleton." [11]
Rinconsaurus [8] R. cadamirus [8]
Titanosaurus [8] Indeterminate [8] Titanosaurus is now considered a nomen dubium.[ citation needed]
Unenlagia [8] U. comahuensis [8] "Fragmentary postcrania." [12]

See also

References

  1. ^ Garrido, 2011, p.237
  2. ^ Garrido, 2011, p.236
  3. ^ Balgord & Carapa, 2014, p.6
  4. ^ Balgord, 2017, p.455
  5. ^ Lebinson et al., 2018, p.252
  6. ^ Leanza et al., 2004, p.63
  7. ^ Weishampel, 2004, pp. 600-604
  8. ^ a b c d e f g h i j k l m n "Río Neuquén Formation." Weishampel, et al. (2004). Pg. 603.
  9. ^ "Table 13.1," in Weishampel, et al. (2004). Page 270.
  10. ^ "Table 10.1," in Weishampel, et al. (2004). Page 199.
  11. ^ "Table 11.1," in Weishampel, et al. (2004). Page 211.
  12. ^ "Table 10.1," in Weishampel, et al. (2004). Page 198.

Bibliography

  • Balgord, Elizabeth A (2017), "Triassic to Neogene evolution of the south-central Andean arc determined by detrital zircon U-Pb and Hf analysis of Neuquén Basin strata, central Argentina (34°S–40°S)", Lithosphere, 9 (3): 453–462, doi: 10.1130/L546.1
  • Balgord, Elizabeth A.; Carapa, Barbara (2014), "Basin evolution of Upper Cretaceous–Lower Cenozoic strata in the Malargüe fold-and-thrust belt: northern Neuquen Basin, Argentina" (PDF), Basin Research: 1–24, retrieved 2019-02-22
  • Garrido, Alberto C (2011), El Grupo Neuquén (Cretácico Tardío) en la Cuenca Neuquina, XVIII Congreso Geológico Argentino, pp. 231–244, retrieved 2019-02-23
  • Leanza, H.A.; Apesteguia, S.; Novas, F.E.; De la Fuente, M.S. (2004), "Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages", Cretaceous Research, 25: 61–87, Bibcode: 2004CrRes..25...61L, doi: 10.1016/j.cretres.2003.10.005, retrieved 2019-02-16
  • Lebinson, Fernando; Turienzo, Martín; Sánchez, Natalia; Araujo, Vanesa; D'Annunzio, María Celeste; Dimieri, Luis (2018), "The structure of the northern Agrio fold and thrust belt (37°30' S), Neuquén Basin, Argentina", Andean Geology, 45 (2): 249–273, doi: 10.5027/andgeoV45n2-3049, hdl: 11336/83841, retrieved 2019-02-22
  • Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN  0-520-24209-2, retrieved 2019-02-21

rio+neuquen+formation Latitude and Longitude:

37°24′S 69°06′W / 37.4°S 69.1°W / -37.4; -69.1
From Wikipedia, the free encyclopedia
(Redirected from Rio Neuquen Formation)
Río Neuquén Subgroup
Stratigraphic range: Late Turonian- Late Coniacian
~91–86  Ma
O
S
D
C
P
T
J
K
N
Type Subgroup
Unit of Neuquén Group
Sub-units Plottier, Sierra Barrosa, Los Bastos & Portezuelo Formations
Underlies Río Colorado Subgroup
Overlies Río Limay Subgroup
ThicknessUp to 155 m (509 ft)
Lithology
Primary Sandstone
Other Claystone, limestone, mudstone
Location
Coordinates 37°24′S 69°06′W / 37.4°S 69.1°W / -37.4; -69.1
Approximate paleocoordinates 42°12′S 49°24′W / 42.2°S 49.4°W / -42.2; -49.4
Region Mendoza, Río Negro & Neuquén Provinces
Country  Argentina
Extent Neuquén Basin
Type section
Named for Neuquén River
Río Neuquén Subgroup is located in Argentina
Río Neuquén Subgroup
Río Neuquén Subgroup (Argentina)

The Río Neuquén Subgroup is a geological subgroup in the Neuquén Basin, Neuquén Province, Argentina, whose strata date back to the Late Cretaceous. The subgroup, formerly defined as a formation, is the middle unit of the Neuquén Group and contains the Plottier, Sierra Barrosa Formation, [1] Los Bastos Formation, [2] and Portezuelo Formations. [3] [4] [5] The subgroup overlies the Río Limay Subgroup and is overlain by the Río Colorado Subgroup. [6] Dinosaur remains are among the fossils that have been recovered from the formation. [7]

Fossil content

Dinosaurs
Genus Species Location Stratigraphic position Material Notes Images
Antarctosaurus [8] A. giganteus [8] "[Two] femora, pubis." [9] Río Neuquén remains previously referred to A. giganteus are now attributed to an indeterminate sauropod. [8]
A. wichmannianus [8]
Megaraptor [8] M. namunhuaiquii [8] "Partial forelimb, manus, and pes." [10]
Patagonykus [8] P. puertai [8] "Partial postcranial skeleton." [11]
Rinconsaurus [8] R. cadamirus [8]
Titanosaurus [8] Indeterminate [8] Titanosaurus is now considered a nomen dubium.[ citation needed]
Unenlagia [8] U. comahuensis [8] "Fragmentary postcrania." [12]

See also

References

  1. ^ Garrido, 2011, p.237
  2. ^ Garrido, 2011, p.236
  3. ^ Balgord & Carapa, 2014, p.6
  4. ^ Balgord, 2017, p.455
  5. ^ Lebinson et al., 2018, p.252
  6. ^ Leanza et al., 2004, p.63
  7. ^ Weishampel, 2004, pp. 600-604
  8. ^ a b c d e f g h i j k l m n "Río Neuquén Formation." Weishampel, et al. (2004). Pg. 603.
  9. ^ "Table 13.1," in Weishampel, et al. (2004). Page 270.
  10. ^ "Table 10.1," in Weishampel, et al. (2004). Page 199.
  11. ^ "Table 11.1," in Weishampel, et al. (2004). Page 211.
  12. ^ "Table 10.1," in Weishampel, et al. (2004). Page 198.

Bibliography

  • Balgord, Elizabeth A (2017), "Triassic to Neogene evolution of the south-central Andean arc determined by detrital zircon U-Pb and Hf analysis of Neuquén Basin strata, central Argentina (34°S–40°S)", Lithosphere, 9 (3): 453–462, doi: 10.1130/L546.1
  • Balgord, Elizabeth A.; Carapa, Barbara (2014), "Basin evolution of Upper Cretaceous–Lower Cenozoic strata in the Malargüe fold-and-thrust belt: northern Neuquen Basin, Argentina" (PDF), Basin Research: 1–24, retrieved 2019-02-22
  • Garrido, Alberto C (2011), El Grupo Neuquén (Cretácico Tardío) en la Cuenca Neuquina, XVIII Congreso Geológico Argentino, pp. 231–244, retrieved 2019-02-23
  • Leanza, H.A.; Apesteguia, S.; Novas, F.E.; De la Fuente, M.S. (2004), "Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages", Cretaceous Research, 25: 61–87, Bibcode: 2004CrRes..25...61L, doi: 10.1016/j.cretres.2003.10.005, retrieved 2019-02-16
  • Lebinson, Fernando; Turienzo, Martín; Sánchez, Natalia; Araujo, Vanesa; D'Annunzio, María Celeste; Dimieri, Luis (2018), "The structure of the northern Agrio fold and thrust belt (37°30' S), Neuquén Basin, Argentina", Andean Geology, 45 (2): 249–273, doi: 10.5027/andgeoV45n2-3049, hdl: 11336/83841, retrieved 2019-02-22
  • Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN  0-520-24209-2, retrieved 2019-02-21

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