Rodent-flea-plague relationships at the higher elevations of San Diego County, California.

Rodent-flea-plague relationships were examined at sites located at higher elevations of San Diego County during 1991-2002. The most frequently sampled rodents were the California ground squirrel, Spermophilus beecheyi, and white-footed mice, Peromyscus spp. Higher seasonal mean dependent variables (prevalences of squirrels and indices of O. montana), higher mean amounts of seasonal rainfall, and lower seasonal mean ambient temperatures were found at sites during 1991--1993 compared with 2000--2002. Levels of plague antibody indicate that squirrels seroconverted at most sites during spring/early summer when exposed to infected fleas when cleaning out burrows following hibernation, when interacting more with other squirrels occurred establishing home ranges, and when dispersing juveniles occupied abandoned burrows containing old nests. The majority of squirrels (35/41) were reported seropositive at Heise County Park (elev. 1,281 m) during 1996, 2001, and 2002. This may reflect fewer fleas biting squirrels more often when squirrels spent more time below-ground in order to avoid higher ambient temperatures. In contrast, most squirrels (12/13) were reported seropositive at two higher sites (elev. 1,584 and 1,641 m) on Palomar Mountain during 1993--1996 when there were higher mean dependent variables and amounts of seasonal rainfall compared with 1999--2002. This increased rainfall may have benefited host and flea populations and thus plague transmission. Seasonal indices were usually reduced after dusting squirrel burrows with 2% diazinon dust. Findings also indicated that S. beecheyi is a primary reservoir for plague at the higher elevations of these and other sites in southern California, and that the deer mouse, Peromyscus maniculatus, and other Peromyscus spp. were not major host reservoirs at the sites sampled.     

Inundation effects on small-scale plant distributions in San Diego, California vernal pools

California vernal pools were used to develop and test hypotheses related to species response patterns and distributions along environmental moisture and elevation gradients. Data from three rainfall years were examined for patterns of plant distribution in relation to length and frequency of inundation and relative elevation. Field distributions on elevation and inundation duration gradients were characteristic of each species, with species distributions overlapping along the gradient. Plants with limited inundation tolerance (`Non-Pool' species) responded to wet years by shifting their distributions toward the dry end of the moisture gradient and in the dry year toward the wetter end. These species have most of their distribution outside of pools. Species with limited tolerance to the gradient extremes had their peak frequency in intermediate positions (`Edge' species). `Pool' species had substantial inundation tolerance. Several were near the limits of inundation tolerance in the deepest study pools, but others withstood longer inundation. `Pool' species had static distributions on the elevation gradient, growing in whatever conditions prevailed in a particular year. A number of annual `Pool' species had their highest frequency in the intermediate, moderately wet year. The dry year had a strong negative effect on the frequency of a few `Pool' annuals, but established perennials persisted regardless. In general, results of the regression analyses can be understood given the other information available on pool hydrology and vegetation. They do not produce any obvious hypotheses to test. For a given species, variables have different predictive value, depending on the year.     

History of kelp beds (Macrocystis) in Orange and San Diego Counties,California

Areas of Macrocystis canopies, as recorded by infrared aerial photography, are presented for about 140 km of the southern California coastline for the 25 year period 1967 to 1991. Several surveys per year were conducted and the largest size canopy per year was selected for presentation. Possible effects from various influences were examined: El Nino and La Nina episodes, storms, rainfall, and human-associated influences such as discharged wastewaters.     

New notharctine (primates,adapiformes) skull from the Uintan (middle Eocene) of San Diego County,California

A new genus and species of notharctine primate, Hesperolemur actius, is described from Uintan (middle Eocene) aged rocks of San Diego County, California. Hesperolemur differs from all previously described adapiforms in having the anterior third of the ectotympanic anulus fused to the internal lateral wall of the auditory bulla. In this feature Hesperolemur superficially resembles extant cheirogaleids. Hesperolemur also differs from previously known adapiforms in lacking bony canals that transmit the internal carotid artery through the tympanic cavity. Hesperolemur, like the later occurring North American cercamoniine Mahgarita stevensi, appears to have lacked a stapedial artery. Evidence from newly discovered skulls of Notharctus and Smilodectes, along with Hesperolemur, Mahgarita, and Adapis, indicates that the tympanic arterial circulatory pattern of these adapiforms is characterized by stapedial arteries that are smaller than promontory arteries, a feature shared with extant tarsiers and anthropoids and one of the characteristics often used to support the existence of a haplorhine-strepsirhine dichotomy among extant primates. The existence of such a dichotomy among Eocene primates is not supported by any compelling evidence. Hesperolemur is the latest occurring notharctine primate known from North America and is the only notharctine represented among a relatively diverse primate fauna from southern California. The coastal lowlands of southern California presumably served as a refuge area for primates during the middle and later Eocene as climates deteriorated in the continental interior. Hesperolemur probably was an immigrant taxon that entered California from either the northern (Wyoming/Utah) or southern (New Mexico) western interior during the middle Eocene © 1995 Wiley-Liss, Inc.