Earliest Arikareean (later early Oligocene) Iniyoo local Fauna from Chilapa formation of Santiago Yolomécatl area in northwestern Oaxaca, southern Mexico

Author(s):  
Eduardo Jiménez-Hidalgo ◽  
E. Bruce Lander ◽  
Isabel Israde-Alcántara ◽  
Nadia Wendoline Rodríguez-Caballero ◽  
Rosalía Guerrero-Arenas
2011 ◽  
Vol 14 (1) ◽  
pp. 15-28 ◽  
Author(s):  
Eduardo Jiménez-Hidalgo ◽  
Rosalía Guerrero-Arenas ◽  
Bruce MacFadden ◽  
Lucía Cabrera-Pérez

1986 ◽  
Vol 60 (4) ◽  
pp. 920-951 ◽  
Author(s):  
Larry G. Marshall ◽  
Richard L. Cifelli ◽  
Robert E. Drake ◽  
Garniss H. Curtis

Fossil land mammals were collected by G. G. Simpson in 1933–1934 at and near the Tapera de López in central Chubut Province, Patagonia, southern Argentina, from rocks now mapped as the Sarmiento Formation. These fossils are assigned to land mammal faunas of Casamayoran (Early Eocene), Mustersan (Middle Eocene), and Deseadan (late Early Oligocene through Early Miocene) age.40K-40Ar age determinations of eight basalt and two tuff units associated with the Deseadan age local fauna at Scarritt Pocket establish a geochronologic framework that calibrates the biostratigraphic record at this locality. The radioisotope dates obtained at Scarritt Pocket range from 23.4 Ma to about 21.0 Ma, and equate with earliest Miocene time. The Scarritt Pocket local fauna is the youngest dated Deseadan age fauna yet known in South America.Seven other localities have, or were reputed to have, local faunas of Deseadan age associated with dated volcanic units. Six of these localities are in Argentina (Gran Barranca, Cerro Blanco, Valle Hermoso, Pico Truncado, Cañadón Hondo, Quebrada Fiera de Malargüe) and one in Bolivia (Estratos Salla in the Salla-Luribay Basin). The stratigraphic relationships of the volcanic units with these local faunas is discussed, and the taxonomic content of each is reassessed.The Deseadan Land Mammal Age is defined by the earliest record of the land mammal genus Pyrotherium, which is from below a basalt dated at 33.6 Ma at Pico Truncado. Other early records of Pyrotherium occur below basalts dated at about 29 Ma at the Gran Barranca and Valle Hermoso, and from a 28.5 Ma level of the Estratos Salla. Thus, the lower boundary for Deseadan time is about 34 Ma.The youngest record of Pyrotherium is in the upper levels of the Estratos Salla dated at about 24 Ma. However, the Scarritt Pocket local fauna, which lacks Pyrotherium, permits placement of the upper boundary for Deseadan time at about 21.0 Ma. Late Deseadan time is surely, and the end of Deseadan time is apparently, marked by the last record of such groups as Proborhyaeninae (Proborhyaena), Rhynchippinae (Rhynchippus), Archaeohyracidae (Archaeohyrax), and the genera Platypittamys (Octodontidae), Scarrittia (Leontiniidae), Propachyrucos and Prohegetotherium (Hegetotheriidae), and Argyrohyrax (Interatheriidae), as these taxa are recorded in the Scarritt Pocket local fauna. Thus, Deseadan time extends from about 34.0 Ma to about 21.0 Ma, making it the Land Mammal Age with the longest known duration in South America.


1994 ◽  
Vol 31 (8) ◽  
pp. 1335-1341 ◽  
Author(s):  
John E. Storer

The Kealey Springs West (KSW) local fauna from the Cypress Hills Formation (Eocene to Miocene), Saskatchewan, is probably latest Chadronian in age, and is the northernmost assemblage representing a time near the Eocene–Oligocene boundary in North America. Presence of Pseudocylindrodon neglectus is strong evidence that the assemblage is Chadronian. Herpetotherium valens, Protosciurus, Namatomys cf. N. lloydi, and Centimanomys also suggest a Chadronian age. The assemblage contains Adjidaumo maximus and Palaeolagus cf. P. hemirhizis, species that have been cited as characteristic of the early part of the Orellan Land Mammal Age (early Oligocene), and the typically Orellan Heliscomys hatcheri and Eumys elegans. Several other tara in the KSW assemblage are known from both the Chadronian (late Eocene) and Orellan.


2011 ◽  
Vol 54 (13) ◽  
pp. 1475-1496 ◽  
Author(s):  
Laura Mori ◽  
Dante J. Morán-Zenteno ◽  
Barbara M. Martiny ◽  
Enrique A. González-Torres ◽  
María Chapela-Lara ◽  
...  

2020 ◽  
Vol 94 (6) ◽  
pp. 1191-1201
Author(s):  
Elizabeth Ortiz-Caballero ◽  
Eduardo Jiménez-Hidalgo ◽  
Victor M. Bravo-Cuevas

AbstractA new species of gopher, Gregorymys mixtecorum n. sp., is described from the Arikareean 1 (early Oligocene) of Oaxaca, southern Mexico. Phylogenetic analysis indicates that it is the sister species of G. veloxikua, which was also recently described from southern Mexico. Both species were collected from sediments of the Chilapa Formation that crop out in northwestern Oaxaca. Gregorymys mixtecorum n. sp. and G. veloxikua show differences in size and proportions that possibly reduced competition for resources, exploiting different microhabitats. Both Mexican species represent the oldest and the most southern records of Gregorymys in North America. The Mexican record of Gregorymys suggests that at least some entoptychine rodents diversified in southern Mexico or Central America, and that Geomyidae has had a wide geographic distribution in North America since the early Oligocene.UUID: http://zoobank.org/0f4ad549-2f59-442b-87fa-5c9be0573ea4


2016 ◽  
Vol 13 (1) ◽  
pp. 131-143
Author(s):  
Julie Boyles

An ethnographic case study approach to understanding women’s actions and reactions to husbands’ emigration—or potential emigration—offers a distinct set of challenges to a U.S.-based researcher.  International migration research in a foreign context likely offers challenges in language, culture, lifestyle, as well as potential gender norm impediments. A mixed methods approach contributed to successfully overcoming barriers through an array of research methods, strategies, and tactics, as well as practicing flexibility in data gathering methods. Even this researcher’s influence on the research was minimized and alleviated, to a degree, through ascertaining common ground with many of the women. Research with the women of San Juan Guelavía, Oaxaca, Mexico offered numerous and constant challenges, each overcome with ensuing rewards.


2006 ◽  
Vol 3 (1) ◽  
pp. 15-25 ◽  
Author(s):  
Jeffrey H. Cohen ◽  
Bernardo Rios ◽  
Lise Byars

Rural Oaxacan migrants are defined as quintessential transnational movers, people who access rich social networks as they move between rural hometowns in southern Mexico and the urban centers of southern California.  The social and cultural ties that characterize Oaxacan movers are critical to successful migrations, lead to jobs and create a sense of belonging and shared identity.  Nevertheless, migration has socio-cultural, economic and psychological costs.  To move the discussion away from a framework that emphasizes the positive transnational qualities of movement we focus on the costs of migration for Oaxacans from the state’s central valleys and Sierra regions.   


2017 ◽  
Vol 4 ◽  
pp. 55-98
Author(s):  
Kathleen Springer ◽  
Jeffrey Pigati ◽  
Eric Scott

Tule Springs Fossil Beds National Monument (TUSK) preserves 22,650 acres of the upper Las Vegas Wash in the northern Las Vegas Valley (Nevada, USA). TUSK is home to extensive and stratigraphically complex groundwater discharge (GWD) deposits, called the Las Vegas Formation, which represent springs and desert wetlands that covered much of the valley during the late Quaternary. The GWD deposits record hydrologic changes that occurred here in a dynamic and temporally congruent response to abrupt climatic oscillations over the last ~300 ka (thousands of years). The deposits also entomb the Tule Springs Local Fauna (TSLF), one of the most significant late Pleistocene (Rancholabrean) vertebrate assemblages in the American Southwest. The TSLF is both prolific and diverse, and includes a large mammal assemblage dominated by Mammuthus columbi and Camelops hesternus. Two (and possibly three) distinct species of Equus, two species of Bison, Panthera atrox, Smilodon fatalis, Canis dirus, Megalonyx jeffersonii, and Nothrotheriops shastensis are also present, and newly recognized faunal components include micromammals, amphibians, snakes, and birds. Invertebrates, plant macrofossils, and pollen also occur in the deposits and provide important and complementary paleoenvironmental information. This field compendium highlights the faunal assemblage in the classic stratigraphic sequences of the Las Vegas Formation within TUSK, emphasizes the significant hydrologic changes that occurred in the area during the recent geologic past, and examines the subsequent and repeated effect of rapid climate change on the local desert wetland ecosystem.


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