Ecologia Alimenticia de la Trucha Arcoiris (Oncorhynchus mykiss nelsoni) del Arroyo San Rafael, Sierra San Pedro Martir, Baja California, Mexico

1992 ◽  
Vol 37 (2) ◽  
pp. 166
Author(s):  
Gorgonio Ruiz-Campos ◽  
Patricia Cota-Serrano
Check List ◽  
2015 ◽  
Vol 11 (3) ◽  
pp. 1649 ◽  
Author(s):  
Jorge Heriberto Valdez-Villavicencio ◽  
Anny Peralta-Garcia ◽  
Bradford Damion Hollingsworth

We found a new population of Ensatina klauberi in San Quintín volcanic field, Baja California. It represents the first coastal population of this species. This record extends the species range ca. 71 km southwest of the southernmost record of E. klauberi in the Sierra San Pedro Mártir and represents the first population discovered outside of coniferous and pine-oak woodlands.


2011 ◽  
Vol 75 (3) ◽  
pp. 647-657 ◽  
Author(s):  
Camille A. Holmgren ◽  
Julio L. Betancourt ◽  
Kate A. Rylander

AbstractPlant macrofossils from 38 packrat middens spanning the last ~ 33,000 cal yr BP record vegetation between ~ 650 and 900 m elevation along the eastern escarpment of the Sierra San Pedro Mártir, northern Baja California. The middens span most of the Holocene, with a gap between ~ 4600 and 1800 cal yr BP, but coverage in the Pleistocene is uneven with a larger hiatus between 23,100 and 14,400 cal yr BP. The midden flora is relatively stable from the Pleistocene to Holocene. Exceptions include Pinus californiarum, Juniperus californica and other chaparral elements that were most abundant > 23,100 cal yr BP and declined after 14,400 cal yr BP. Despite being near the chaparral/woodland-desertscrub ecotone during glacial times, the midden assemblages reflect none of the climatic reversals evident in the glacial or marine record, and this is corroborated by a nearby semi-continuous pollen stratigraphy from lake sediments. Regular appearance of C4 grasses and summer-flowering annuals since 13,600 cal yr BP indicates occurrence of summer rainfall equivalent to modern (JAS average of ~ 80–90 mm). This casts doubt on the claim, based on temperature proxies from marine sediments in the Guaymas Basin, that monsoonal development in the northern Gulf and Arizona was delayed until after 6200 cal yr BP.


2013 ◽  
Vol 118 (4) ◽  
pp. 1660-1673 ◽  
Author(s):  
D. M. Meko ◽  
R. Touchan ◽  
J. Villanueva Díaz ◽  
D. Griffin ◽  
C. A. Woodhouse ◽  
...  

2021 ◽  
Vol 80 (2) ◽  
Author(s):  
Iván Alejandro Meza-Matty ◽  
Gorgonio Ruiz-Campos ◽  
Luis Walter Daesslé ◽  
Arturo Ruiz-Luna ◽  
Álvaro Alberto López-Lambraño ◽  
...  

The present study measured the daily, seasonal, and annual variability of the water temperature of streams in which the endemic rainbow trout, Oncorhynchus mykiss nelsoni, is distributed on the western slope of the Sierra San Pedro Mártir, Baja California, Mexico, between 1996 and 2019. The seasonal thermal interval and daily duration of summer temperatures above the thermal threshold for this trout subspecies (≥ 28°C) were determined in streams at different elevations (553, 1,220, and 2,080 masl, or meters above sea level). Temperatures ≥ 28°C were recorded at the study site on the stream with the lowest elevation (San Antonio de Murillos Creek) over an accumulated 365 h between June and September 2014, with the maximum temperature recorded there, 30.66 °C, making it the site most vulnerable to climate change. At the San Antonio de Murillos Creek, the average water temperature predicted by three models (GFDL R30, HadCM3, and Mote) for the year 2025 would be a non-lethal temperature, < 28 °C, for trout at a minimum elevation of 491-511 masl, while this was predicted to be 545-701 masl for the year 2050. Predicted hourly water temperatures of 28°C (non-lethal) may occur at minimum elevations of 868-898 masl in 2025 and at 908-1028 masl in 2050, reducing a 21-23% and 23-31% its current altitudinal distribution range, respectively, thus avoiding its presence at the type locality (San Antonio de Murillos).


Author(s):  
R. Gordon Gastil ◽  
David L. Kimbrough ◽  
Joan M. Kimbrough ◽  
Marty Grove ◽  
Masaaki Shimizu

Tectonics ◽  
1989 ◽  
Vol 8 (4) ◽  
pp. 833-844 ◽  
Author(s):  
James E. O'Connor ◽  
Clement G. Chase

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