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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Desmostylians
Figure 2. Three different skeletal reconstructions of desmostylians based ... Available to Purchase
A paleoecological paradox: the habitat and dietary preferences of the extinct tethythere Desmostylus , inferred from stable isotope analysis Available to Purchase
Paleomagnetism and counterclockwise tectonic rotation of the Upper Oligocene Sooke Formation, southern Vancouver Island, British Columbia Available to Purchase
PALEONTOLOGY OF THE MIDDLE MIOCENE LOS INDIOS MEMBER OF THE ROSARITO BEACH FORMATION, NORTHWESTERN BAJA CALIFORNIA, MEXICO Available to Purchase
ABSTRACT Siliceous microfossils, mega-invertebrates and vertebrates are described from the marine Middle Miocene Los Indios Member of the Rosarito Beach Formation. The large and diverse marine vertebrate assemblage of sharks, rays, bony fishes, sea birds, dolphins, cetotheres, pinnipeds, a sea cow and a desmostylian, is here named the La Misiòn Local Fauna. Correlation with the (?)Hemingfordian/(?)Barstovian land mammal ages is tentatively made. Mollusks from the Los Indios Member allow correlation with the “Temblor” provincial molluscan stage, and silicoflagellates indicate a correlation with the Corbisema triacantha Zone, dated in the deep sea at 14-15 million years before present. This date is corroborated by radiometric dates on basalts stratigraphically above (14.3 ± 2.6 million years) and below (16.1 ± 2.1 million years) the Los Indios Member. Preliminary paleoenvironmental analysis indicates that the fossil assemblages of the Los Indios Member lived under open marine, inner shelf conditions with subtropical water temperatures and clear, non-turbid water.
Miocene Vertebrate Geochronology of West Coast of North America Available to Purchase
Depositional Environment and Geologic Age of Neogene Rocks at Cape Aliaksin, Beaver Bay, Alaska Peninsula Available to Purchase
CAUGHT IN THE ACT: TROPHIC INTERACTIONS BETWEEN A 4-MILLION-YEAR-OLD WHITE SHARK ( CARCHARODON ) AND MYSTICETE WHALE FROM PERU Available to Purchase
SHARK-BITTEN PROTOSTEGID TURTLES FROM THE UPPER CRETACEOUS MOOREVILLE CHALK, ALABAMA Available to Purchase
Filling a gap in the proboscidean fossil record: a new genus from the Lutetian of Senegal Available to Purchase
Middle and late Miocene marine mammal assemblages from the Monterey Formation of Orange County, California Available to Purchase
ABSTRACT This study provides new stratigraphic data and identifications for fossil marine mammals from the Monterey Formation in the Capistrano syncline, Orange County, California, showing that there are two distinct marine mammal assemblages. Until now, marine mammals from the Monterey Formation of Orange County have been considered to represent a single assemblage that is 13.0–10.0 Ma in age. By combining data from diatoms with the geographic positions of sites, faunal analysis, and data from the literature, we can assign 59 sites to three main levels: the lower part (ca. 16–13 Ma), the middle part (ca. 13–10 Ma), and the upper part (ca. 10–8 Ma). We assigned 308 marine mammal specimens to 38 taxa, resulting in 97 occurrences (unique record of a taxon for a given site). Of the 38 taxa we identified within the study area, 15 taxa are restricted to the lower part of the Monterey Formation, 15 are restricted to the upper part of the Monterey Formation, eight were found in both, and none has yet been reported from the middle (possibly condensed) section. Six of the eight taxa that occur in both the lower and upper parts of the Monterey Formation are higher-level taxa, which accounts for their broad temporal range. The recognition of two distinct marine mammal assemblages in the Monterey Formation of Orange County is an important step toward a better-calibrated sequence of faunal evolution in the region while improving the utility of marine mammals for regional biostratigraphy.