THE ENVIRONMENTAL CONTEXT OF CHANGING MAMMAL DIVERSITY THROUGH THE MIDDLE MIOCENE CLIMATIC OPTIMUM IN THE BARSTOW FORMATION, MOJAVE DESERT, CALIFORNIA

2019 ◽  
Author(s):  
Katharine M. Loughney ◽  
◽  
Michael T. Hren ◽  
Selena Y. Smith ◽  
Janice L. Pappas ◽  
...  
2019 ◽  
Vol 132 (1-2) ◽  
pp. 113-129 ◽  
Author(s):  
Katharine M. Loughney ◽  
Michael T. Hren ◽  
Selena Y. Smith ◽  
Janice L. Pappas

Abstract The Barstow Formation (ca. 19–13 Ma) of southern California, USA, is a terrestrial sequence known for its diverse Miocene mammalian faunas. The formation spans the Middle Miocene Climatic Optimum (MMCO; 17–14 Ma) and offers the opportunity to study environmental change during the last major interval of global warming of the Cenozoic. We combined isotopic analyses of carbon and hydrogen from sedimentary n-alkanes and bulk soil organic matter with analysis of phytoliths (plant silica) and diatoms to reconstruct vegetation composition, habitat structure, and moisture dynamics through the formation. The δ13C and δD of long-carbon-chain n-alkanes derived from terrestrial plants and preserved in sediments of the Barstow Formation record drying prior to the MMCO and through the Middle Miocene Climatic Transition (MMCT; beginning ca. 14 Ma), punctuated by increased moisture in fluvial environments during the peak of the MMCO. Variable isotopic results relate to changes in moisture, driven partly by facies, vegetation composition, tectonic activity, and climatic variability coinciding with intervals of high pCO2. Phytolith assemblages are dominated by forest indicators in riparian habitats during the MMCO, and grass morphotypes constitute significant components of phytolith assemblages after the MMCO, indicating a shift to drier, more open-canopy habitats. The establishment of dry, wooded grasslands in the Barstow Basin coincides with the beginning of the MMCT and cooling sea-surface temperatures in the Pacific Ocean. Our results indicate that moist, closed-canopy habitats formed in southern California during climatic warming, followed by savannah during climatic cooling and the shift to seasonal precipitation regimes.


Geology ◽  
2001 ◽  
Vol 29 (2) ◽  
pp. 139 ◽  
Author(s):  
Mona L. Becker ◽  
Jennifer M. Cole ◽  
E. Troy Rasbury ◽  
Vicki A. Pedone ◽  
Isabel P. Montañez ◽  
...  

2020 ◽  
Author(s):  
Julian F. Quintero-Galvis ◽  
Pablo Saenz-Agudelo ◽  
Juan L. Celis-Diez ◽  
Guillermo C. Amico ◽  
Soledad Vazquez ◽  
...  

AbstractAimSeveral geological events affecting Southern South America during the middle Miocene climatic optimum acted as important drivers of diversification to the biota. This is the case of Microbiotheria, for which Dromiciops is considered the sole surviving lineage, the sister group of Eomarsupialia (Australian marsupials). Three main Dromiciops genetic lineages are known, whose divergence was initially attributed to recent Pleistocene glaciations. Using fossil-calibrated dating on nuclear and mitochondrial genes, here we reevaluate this hypothesis and report an older (Miocenic) biogeographic history for the genus.LocationSouthern South America.MethodsPhylogenetic reconstruction using sequences from two mitochondrial DNA and four nuclear DNA genes in 159 specimens, from 31 sites across Chile and Argentina. Divergence time estimation using fossil calibration.ResultsOur phylogenetic analysis resolved four well supported clades with discrete geographic distributions. The oldest and most differentiated clade corresponds to that of the northern distribution (35.2°S to 39.3°S), which would be a different species (D. bozinovici, sensu D’elia et al. 2016). According to our estimations, this species shared a common ancestor with D. gliroides (southern clades) about 13 million years ago (95% CI: 6.4-25.3). The southern clades (39.6°S to 42.0°S), showed a divergence time ranging from 9.57 to 6.5 Mya. Strong genetic structure was detected from north to south but not across the Andes, or between Chiloé island/ mainland. Demographic equilibrium is inferred to the northern clade, and recent demographic expansions was detected in the central and southern clades.Main conclusionsThe whole diversification of Dromiciops occurred within the Miocene, being the Middle Miocene transgression (MMT), the massive marine flooding that covered several lowlands of the western face of los Andes between 38-48° S, the most likely diversifying force. This was the result of an increase in global sea levels due to the Miocene climatic optimum, which shaped the biogeographic origin of several species, including Nothofagus forests, the habitat main of Dromiciops.


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