Bolomor Cave (Level IV)
Basic information
Sample name: Bolomor Cave (Level IV)
Reference: R. Blasco and J. F. Peris. 2012. A uniquely broad spectrum diet during the Middle Pleistocene at Bolomor Cave (Valencia, Spain). Quaternary International 252:16-31 [ER 3896]
Geography
Country: Spain
State: Valencia
Coordinate: 39.072926° N, -0.269804° W
Coordinate basis: estimated from map
Time interval: Middle Pleistocene
Section: IV
Unit order: above to below
Max Ma: 0.152
Min Ma: 0.121
Age basis: other
Geography comments: Bolomor Cave is situated on the "southern slope of the Valldigna valley, approximately 2 km southeast of the town of Tavernes"
The coordinates entered are based on Tavernes de la Valldigna as that was the closest possible estimate
"The karst deposit of Bolomor Cave has been dated by Amino Acid Racemization (AR) and Thermoluminescence (TL) to between MIS 9 and MIS 5"
No specific date is provided for Level IV though it is situated multiple layers above Level XII which is dated to 0.152 Ma +/- 0.023 Ma and two layers below Level II which is dated to 0.121 Ma +/- 0.018
The coordinates entered are based on Tavernes de la Valldigna as that was the closest possible estimate
"The karst deposit of Bolomor Cave has been dated by Amino Acid Racemization (AR) and Thermoluminescence (TL) to between MIS 9 and MIS 5"
No specific date is provided for Level IV though it is situated multiple layers above Level XII which is dated to 0.152 Ma +/- 0.023 Ma and two layers below Level II which is dated to 0.121 Ma +/- 0.018
Environment
Lithology: siliciclastic (mixed)
Taphonomic context: carnivore accumulation,cave,human accumulation
Habitat comments: "Bolomor cave is a karst cavity opened to the exterior approximately 500 ka, as a consequence of the erosion of the ravine where is placed"
"The sedimentary sequence of Bolomor Cave consists mainly of allochthonous material of colluvial origin. In addition to these deposits, there are other autochthonous sediments of gravitational origin from the roof subsidence, due to tectonics or weathering processes."
Cut marks are identified on 7.18% of bone remains mainly on the limb bones of medium and large-sized taxa, as well as birds, tortoises, and O. cuniculus
Evidence of burning was found on 61.54% of remains at Level IV mostly on lagomorphs and tortoises
"The sedimentary sequence of Bolomor Cave consists mainly of allochthonous material of colluvial origin. In addition to these deposits, there are other autochthonous sediments of gravitational origin from the roof subsidence, due to tectonics or weathering processes."
Cut marks are identified on 7.18% of bone remains mainly on the limb bones of medium and large-sized taxa, as well as birds, tortoises, and O. cuniculus
Evidence of burning was found on 61.54% of remains at Level IV mostly on lagomorphs and tortoises
Methods
Life forms: carnivores,primates,ungulates,other small mammals,birds,turtles,frogs,fishes
Sampling methods: quarry
Sample size: 2778 specimens
Sampling comments: Excavated between 1991-1998 and 2005
2864 of the 25323 remains found at Level IV were taxonomically identified
30 taxa were identified at Level IV
Counts excluded:
Carnivora indet. - 5
Aves indet. - 17
Passeriformes - 25
Corvidae - 20
Galliformes - 19
2864 of the 25323 remains found at Level IV were taxonomically identified
30 taxa were identified at Level IV
Counts excluded:
Carnivora indet. - 5
Aves indet. - 17
Passeriformes - 25
Corvidae - 20
Galliformes - 19
Metadata
Sample number: 4280
Contributor: Jack Nesbitt
Enterer: Jack Nesbitt
Created: 2023-05-23 11:57:04
Modified: 2023-05-23 02:10:45
Abundance distribution
25 species
3 singletons
total count 2778
extrapolated richness: 33.4
Fisher's α: 3.789
geometric series k: 0.7573
Hurlbert's PIE: 0.8173
Shannon's H: 2.0400
Good's u: 0.9989
Each square represents a species. Square sizes are proportional to counts.
• Find matching samples
Register
| Macaca sylvanus | 1 | |
| "Macaca sylvana" | ||
| Ursus arctos | 1 | 156 kg frugivore-carnivore |
| Canis lupus | 2 | 43 kg carnivore |
| Vulpes vulpes | 2 | 5.3 kg carnivore-insectivore |
| Panthera sp. | 3 | |
| "Panthera leo": no details are given, so it is unclear whether this might be Panthera spelaea | ||
| Lynx pardinus | 2 | 11 kg |
| "Lynx pardina" | ||
| Palaeoloxodon antiquus | 4 | |
| "Paleoloxodon antiquus" | ||
| Equus ferus | 65 | 422 kg |
| Equus hemionus hydruntinus | 16 | grazer |
| "Equus hydruntinus" | ||
| Hippopotamus amphibius | 46 | 1107 kg grazer |
| Sus scrofa | 115 | 54 kg herbivore |
| Dama sp. | 91 | |
| Cervus elaphus | 647 | 104 kg |
| Bos primigenius | 213 | |
| Hemitragus cedrensis | 121 | |
| Oryctolagus cuniculus | 789 | 2.5 kg browser-grazer |
| Pyrrhocorax sp. | 6 | |
| "Phyrrocorax sp." | ||
| Phasianidae indet. | 24 | |
| Columba sp. | 34 | |
| Anas sp. | 29 | |
| Aythya sp. | 34 | |
| Strigidae indet. | 1 | |
| Testudo hermanni | 526 | |
| Bufo sp. | 4 | |
| Salmonidae indet. | 2 | |
Current reference:
Huckleberry et al. 2001 (ER 3215)