Headwaters of the Rio Chico, Lago Colhue Huapi: Coniacian - Maastrichtian, Argentina
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
- Hadrosauridae
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Ibiricu et al. 2019 | 1 element | |||||||||
UNPSJB PV 1050/1061, dentary fragment and partial skeleton | ||||||||||
unclassified
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The relative abundance was based on counts of 300 specimens | ||||||||||
Marchantiopsida
- Marchantiidae
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Zlivisporis reticulatus
(Playford 1971)
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The relative abundance was based on counts of 300 specimens | ||||||||||
unclassified
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Interulobites intraverrucatus
Phillips 1971
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The relative abundance was based on counts of 300 specimens | ||||||||||
Lycopodiopsida
- Selaginellales
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Ceratosporites equalis
Cookson and Dettmann 1958
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The relative abundance was based on counts of 300 specimens | ||||||||||
The relative abundance was based on counts of 300 specimens | ||||||||||
Algae
- Zygnemataceae
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Ovoidites sp.
Krutzsch 1959
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The relative abundance was based on counts of 300 specimens | ||||||||||
Catinipollis geiseltalensis
Krutzch 1966
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The relative abundance was based on counts of 300 specimens | ||||||||||
unclassified
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Cycadopites sp.
Wodehouse 1933
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The relative abundance was based on counts of 300 specimens | ||||||||||
Magnoliopsida
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Echimonocolpites sp.
der Hammen and de Mutis 1965
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The relative abundance was based on counts of 300 specimens | ||||||||||
Quadraplanus brossus
Stover and Partridge 1973
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Arecaceae
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Liliaceae
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Liliacidites cf. kaitangataensis
Couper 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Araceae
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Proxapertites sp.
Van der Hammen 1956
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Proteales
- Proteaceae
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Proteacidites scaboratus
Couper 1960
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The relative abundance was based on counts of 300 specimens | ||||||||||
Proteacidites cf. scaboratus
Couper 1960
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The relative abundance was based on counts of 300 specimens | ||||||||||
Beaupreaidites orbiculatus
Dettmann and Jarzen 1988
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The relative abundance was based on counts of 300 specimens | ||||||||||
Beaupreaidites cf. elegansiformis
Cookson 1950
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Proteales
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Peninsulapollis gillii
Dettmann and Jarzen 1988
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The relative abundance was based on counts of 300 specimens | ||||||||||
Peninsulapollis truswelliae
Dettmann and Jarzen 1988
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Buxales
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Gunnerales
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Tricolpites sp.
Couper 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Asterales
- Asteraceae
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Tubulifloridites lilliei
Farabee and Canright 1986
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The relative abundance was based on counts of 300 specimens | ||||||||||
Angiospermae
- Ericales
- Ericaceae
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Ericipites scabratus
Harris 1965
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The relative abundance was based on counts of 300 specimens | ||||||||||
Coniferales
- Podocarpaceae
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Podocarpidites spp.
Cookson 1947
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The relative abundance was based on counts of 300 specimens | ||||||||||
The relative abundance was based on counts of 300 specimens | ||||||||||
Microcachryidites antarcticus
Couper 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
unclassified
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Rugubivesiculites sp.
Pierce 1961
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The relative abundance was based on counts of 300 specimens | ||||||||||
Gnetaceaepollenites barghoornii
Lima 1980
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The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Marsileaceae
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The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Schizaeales
- Schizaeaceae
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The relative abundance was based on counts of 300 specimens | ||||||||||
The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Schizaeales
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Ruffordiaspora sp.
Dettmann and Clifford 1992
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The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Salviniales
- Salviniaceae
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The relative abundance was based on counts of 300 specimens | ||||||||||
The relative abundance was based on counts of 300 specimens | ||||||||||
Azolla sp.
Lamarck 1783
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The relative abundance was based on counts of 300 specimens | ||||||||||
Ariadnaesporites micromedusus
Stough 1968
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The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Osmundaceae
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Baculatisporites comaumensis
Potonie 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
Polypodiopsida
- Gleicheniaceae
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Gleicheniidites senonicus
Ross 1949
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The relative abundance was based on counts of 300 specimens | ||||||||||
Pteridopsida
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Cyathidites sp.
Couper 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
Equisetopsida
- Araucariaceae
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The relative abundance was based on counts of 300 specimens | ||||||||||
Equisetopsida
- Cheirolepidiaceae
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Classopollis sp.
Pflug 1953
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The relative abundance was based on counts of 300 specimens | ||||||||||
see common names |
Geography
Country: | Argentina | State/province: | Chubut |
Coordinates: | 45.6° South, 68.4° West (view map) | ||
Paleocoordinates: | 46.6° South, 51.1° West (Wright 2013) | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | small collection |
Time
Period: | Cretaceous | Epoch: | Late Cretaceous |
Stage: | Coniacian - Maastrichtian | 10 m.y. bin: | Cretaceous 6 - Cretaceous 8 |
Key time interval: | Coniacian - Maastrichtian | ||
Age range of interval: | 89.8 - 66 m.y. ago |
Stratigraphy
Geological group: | Chubut | Formation: | Lago Colhué Huapi | ||
Stratigraphic resolution: | bed | ||||
Stratigraphy comments: At the headwaters of the Río Chico, a basalt flow with a radiometric age of 67.31 ± 0.55 Ma (La Angostura Basalt) lies on top of the Lago Colhué Huapi Formation (Clyde et al., 2014) |
Lithology and environment
Primary lithology: | massive,lenticular,planar lamination mudstone |
Includes fossils? | Y |
Lithology description: The Lago Colhué Huapi Formation, widely distributed in the basin, is predominantly composed of reddish mudstones of fluvial origin. According to the position in the basin, the Lago Colhué Huapi Formation overlies the Bajo Barreal Formation and underlies the marine Danian Salamanca Formation or the tuffaceous levels of the Laguna Palacios Formation (Casal et al., 2015). In the upper part of the Lago Colhué Huapi Formation, at the headwaters of the Río Chico, an erosion surface underlies sedimentary rocks including the fertile levels. | |
Environment: | channel lag |
Geology comments: Aquatic fern spores (Azolla spp.; Ariadnaesporites micromedusus) together with lycophytes and algal elements suggest the local existence of a freshwater body and a warm climate. Particularly, zygospores of the green filamentous algae Zygnemataceae such as Catinipollis geiseltalensis Krutzsch, 1966 imply warm, shallow and low energy freshwaters (Scafati et al., 2009; Bowman et al., 2014). |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Spatial orientation: | random |
Preservation of anatomical detail: | good |
Abundance in sediment: | few |
Articulated whole bodies: | none |
Associated major elements: | none |
Disassociated major elements: | many |
Disassociated minor elements: | many |
Fragmentation: | occasional |
Bioerosion: | frequent |
Encrustation: | none |
Temporal resolution: | snapshot |
Spatial resolution: | autochthonous |
Collection methods and comments
Collection excludes: | some macrofossils |
Collection methods: | surface (in situ),chemical,mechanical,hydroflouric,field collection |
Collection size: | 300 specimens |
Reason for describing collection: | general faunal/floral analysis |
Collection method comments: The samples were processed following standard palynological methods including maceration with hydrochloric and hydrofluoric acids for carbonate and silicate removal. A brief oxidation of the residue with nitric acid was performed in order to improve the results. The organic residue was mounted on microscope slides using glycerine jelly. The samples were studied with a Carl Zeiss KF 2 microscope and the microphotographs were obtained with a digital Nikon Coolpix P2 camera at the Biostratigraphic Laboratory of the Universidad Nacional de la Patagonia San Juan Bosco. The relative abundance of palynomorphs mentioned in the analysis of the palynoflora was based on counts of 300 specimens. | |
Taxonomic list comments:UNPSJB, Universidad de la Patagonia “San Juan Bosco”, colección de Paleovertebrados, Chubut, Argentina |
Metadata
Database number: | 233992 | ||
Authorizer: | E. Vlachos | Enterer: | F. Aspromonte | Research group: | paleobotany,vertebrate |
Created: | 2024-03-11 12:22:26 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2024-03-11 12:22:26 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
87794. | P. Vallati, G. Casal, N. Foix, J. Allard, A. De Sosa Tomas and M. Calo. 2016. First report of a Maastrichtian palynoflora from the Golfo San Jorge Basin, central Patagonia, Argentina. Ameghiniana 53(4):495-505 [E. Vlachos/F. Aspromonte] |
Secondary references:
87800 | L. M. Ibiricu, G. A. Casal, B. N. Alvarez, R. D. Martinez, and M. Luna. 2019. Nuevos materiales de Hadrosauridae de la Formación Lago Colhue Huapi, Cretácico Superior, Patagonia Central. Publicación Electrónica de la Asociación Paleontológica Argentina 56-57 [E. Vlachos/F. Aspromonte] |