Hueso Blanco: Tortonian, Peru
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
- Suliformes
- Sulidae
|
|||||||
Reptilia
- Spheniscidae
|
|||||||
Spheniscus sp.
Brisson 1760
|
|||||||
Reptilia
- Gavialidae
|
|||||||
Mammalia
- Nothrotheriidae
|
|||||||
Mammalia
- Cetacea
- Phocoenidae
|
|||||||
Mammalia
- Cetacea
|
|||||||
Balaenopteroidea indet.
(Gray 1868)
|
|||||||
Mammalia
- Carnivora
- Phocidae
|
|||||||
Actinopteri
- Clupeiformes
- Clupeoidei
|
|||||||
Sardinops sp.
Hubbs 1929
|
|||||||
see common names |
Geography
Country: | Peru |
Coordinates: | 15.5° South, 74.8° West (view map) |
Paleocoordinates: | 14.9° South, 72.6° West (Wright 2013) |
Basis of coordinate: | stated in text |
Geographic resolution: | small collection |
Time
Period: | Neogene | Epoch: | Miocene |
Stage: | Tortonian | 10 m.y. bin: | Cenozoic 6 |
Key time interval: | Tortonian | ||
Age range of interval: | 11.63 - 7.246 m.y. ago |
Stratigraphy
Formation: | Pisco | ||||
Regional section: | Brand | Regional bed: | LM 10 | ||
Stratigraphic resolution: | bed | ||||
Stratigraphy comments: Brand et al. (2011) argued that the sediment package exposed at Hueso Blanco (featuring the LM 10 marker bed) is roughly correlative with the El Jahuay (ELJ) vertebrate level of de Muizon and DeVries (1985) and de Muizon (1988). In turn, Lambert and de Muizon (2013) reattributed the LM 10 marker bed to the Aguada de Lomas (AGL) vertebrate level, based on faunal and sedimentary similarities (de Muizon and DeVries, 1985; de Muizon, 1988). Based on K/Ar dating of underlying tuff layers, the AGL vertebrate level is considered younger than 7.93 Ma (about 7.5–7.0 Ma) (de Muizon and DeVries, 1985; de Muizon and Bellon, 1986; Lambert and de Muizon, 2013). Finally, 87Sr/86Sr analyses on marine mollusc shells bracketed the age of the AGL level between 7.46 Ma and 7.30 Ma (Ehret et al., 2012). |
Lithology and environment
Primary lithology: | fine sandstone |
Includes fossils? | Y |
Lithology description: The sediment package exposed at Hueso Blanco (bed LM 10 in Brand et al., 2011) is about 15 m thick and consists mainly of sparsely to moderately bioturbated, well-sorted, fine- to medium- grained sandstones (Electronic supplementary material; Fig. S1). | |
Environment: | marine indet. |
Taphonomy
Modes of preservation: | body,trace |
Size of fossils: | macrofossils |
Feeding/predation traces: | tooth marks |
Collection methods and comments
Reason for describing collection: | paleoecologic analysis |
Metadata
Database number: | 183918 | ||
Authorizer: | M. Uhen | Enterer: | M. Uhen |
Modifier: | M. Kouvari | Research group: | vertebrate |
Created: | 2017-01-18 13:27:11 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2017-01-18 13:27:11 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
61392. | A. Collareta, O. Lambert, W. Landini, C. Di Celma, E. Malinverno, R. M. Varas-Malca, M. Urbina and G. Bianucci. 2017. Did the giant extinct shark Carcharocles megalodon target small prey? Bite marks on marine mammal remains from the late Miocene of Peru. Palaeogeography, Palaeoclimatology, Palaeoecology 469:84-91 [M. Uhen/M. Uhen/O. Alfaro] |