Santa Rosa: Serravallian - Tortonian, Peru

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia - Cetacea - Cetotheriidae
Tiucetus rosae n. gen., n. sp. Marx et al. 2017
1 specimen
MNHN.F. PPI261
see common names

Geography
Country:Peru
Coordinates: 14.8° South, 75.5° West (view map)
Paleocoordinates:15.3° South, 73.0° West
Basis of coordinate:stated in text
Time
Period:Neogene Epoch:Miocene
Key time interval:Serravallian - Tortonian
Age range of interval:13.82000 - 7.24600 m.y. ago
Stratigraphy
Formation:Pisco
Stratigraphy comments: poorly explored lowest part of the Pisco Formation (allomember P0 [23]

The strata that yielded the holotype of Tiucetus rosae rest unconformably on the latest Oligocene to Early Miocene Chilcatay Formation. Sediment samples from the skull, associated specimens and the locality of Santa Rosa itself failed to yield microfossils, and there is currently no other direct dating evidence available for P0. Nevertheless, dates from the underlying Chilcatay Formation and the overlying P1 allomember of the Pisco Formation constrain the deposition of P0 to between 17.8 and 9.0 Ma [23]. Furthermore, dated ash beds from within the P1 and P2 allomembers suggest that both were deposited over no more than 1–1.5 Myr each [23]. Assuming similar rates of sedimentation for P0 would yield an approximate age of 11–9 Ma (Tortonian) for Tiucetus, which is consistent with the occurrence of a ‘typical’ Late Miocene cetotheriid morphotype (i.e. one broadly resembling ‘Cetotherium’ megalophysum and Herentalia) in the same unit.
However, the situation is complicated by an apparent mismatch between faunal and radiometric data from the Pisco-Ica and Sacaco basins. Of particular relevance here is the age of the El Jahuay vertebrate level (ELJ), which is among the oldest vertebrate horizons exposed in the Sacaco Basin, and has been K/Ar-dated to older than 8.8 Ma [18]. Based on its vertebrate fauna, ELJ appears to be stratigraphically above the Cerro La Bruja vertebrate level (CLB) of the Pisco-Ica Basin [18,25,30], yet diatom assemblages and more recent radiometric dates from the localities of Cerro La Bruja and Cerro Los Quesos place CLB between 7.5 and 8.5 Ma [23,31,32]. If CLB has been correctly dated, then a revision of the dating evidence from the Sacaco Basin appears to be in order. Alternatively, if the ELJ estimate is correct, CLB, and indeed all of the Pisco Formation exposed in the Pisco-Ica Basin, may be older than recently suggested [23,31,32]. In this scenario, a conservative estimate for the age of P0 might be late Middle Miocene (Serravallian; 13.8–11.6 Ma), which may be further supported by the markedly archaic aspect of the cetacean assemblage from this unit relative to P1 and P2 (see above).
In the light of these conflicting hypotheses, the age of Tiucetus rosae must fall somewhere between 17.8 and 9.0 Ma, and plausibly within either the Serravallian or the early Tortonian period, depending on the resolution of the mismatch between the Pisco-Ica and Sacaco basins. A Serravallian age is supported by the mainly archaic cetacean assemblage of P0 and radiometric dates from the Sacaco Basin, although the more recent dating evidence from the Pisco-Ica Basin does not exclude the possibility of an early Tortonian age. Direct evidence for the age of P0 and a re-examination of the radiometric data from the Sacaco area are required to resolve this question.
Lithology and environment
Primary lithology: not reported
Environment:marine indet.
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Reason for describing collection:general faunal/floral analysis
Metadata
Database number:188740
Authorizer:M. Uhen Enterer:M. Uhen
Research group:vertebrate
Created:2017-09-14 09:08:14 Last modified:2017-09-14 09:08:14
Access level:the public Released:2017-09-14 09:08:14
Creative Commons license:CC BY
Reference information

Primary reference:

63340. F. G. Marx, O. Lambert, and C. Muizon. 2017. A new Miocene baleen whale from Peru deciphers the dawn of cetotheriids. Royal Society Open Science 4:170560 [M. Uhen/M. Uhen]