The spatial distribution of an organism’s habitat can vary at local, regional, and global scales (Shen et al. 2013: Anderson et al. 2016; Klingler, Jahner et al. 2021). How an organism navigates the spatial structure of its habitat will depend upon its body size, mode of locomotion and life history (Peacock and Smith 1997; Pinto and MacDougall 2010; Wauters et al. 2010; Neam and Lacher 2018). Climate change is likely to alter not only the extent of suitable habitat, but also the spatial organization of occupiable habitat patches for many organisms. As some habitat patches become unsuitable, the distance among inhabitable patches may increase, potentially impeding an organism’s ability to move among otherwise suitable habitat areas. Such a dynamic may spiral into an extinction vortex (Benson et al. 2019) as populations or subpopulations become increasing isolated and subject to demographic and genetic stochasticity (Lande 1993), thereby reducing both persistence probability and evolutionary potential (Blomqvist et al. 2010).
Here we examine the temporal dynamics of patch occupancy and the maintenance of genetic diversity within a population of American pika (Ochotona princeps), a small, thermally sensitive alpine lagomorph considered vulnerable to global warming (Beever et al. 2010; Calkins et al. 2012; Stewart et al. 2015; Schwalm et al. 2016). O. princeps is broadly distributed across mountain ranges of the western United States and Canada (Smith and Weston 1990; Hafner and Smith 2010). Pikas are known to occupy a diversity of rocky habitats including talus patches, lava flows and even hard-rock mining ore dumps (Severaid 1955; Peacock 1997; Peacock and Smith 1997; Rodhouse et al. 2010). Such habitat is naturally fragmented and varies widely in patch size, proximity to other patches and therefore levels of connectivity across the range of this species. Because pikas already sustain a high resting body temperature (40.1°C) very close to their upper lethal temperature (43.1°C), the thermal consistency of the interstitial spaces of rocky talus habitat allows them to adjust their internal temperature through behavioral thermoregulation (MacArther and Wang 1973; Wilkening et al. 2015). This physiological sensitivity combined with a limited dispersal capacity (Smith and Ivins 1983; Peacock 1997) increases pika vulnerability to changing environmental conditions under climate change (Stewart et al. 2017).
Over the past several decades, pika populations have been disappearing, particularly in the mountain ranges of the Great Basin physiographic region, southern Utah, and lower elevation sites on the eastern slopes of the Sierra Nevada (Beever et al. 2003; 2010; 2011; 2016; Stewart and Wright 2012; Nichols et al. 2016; Stewart et al. 2015; 2017). These declines disproportionately affect the subspecies O. princeps schisticeps, whose distribution includes the Sierra Nevada and Great Basin mountain ranges of western and central Nevada (Galbreath et al. 2009; 2010). In addition to evidence of shifts in the elevational distribution of pikas as a result of prehistoric climate change (late Pleistocene (Wisconsinan) to early Holocene; Hafner 1994; Grayson 2005), metrics of temperature measured during 20th and 21st century human mediated climate change have repeatedly been identified as predictors of extant pika distributional change and persistence (Beever et al. 2003; Beever et al. 2010; Calkins et al. 2012; Stewart et al. 2015; Schwalm et al. 2016). However, at smaller spatial scales, non-climatic factors such as habitat configuration, connectivity, and suitable dispersal habitat are also likely to contribute to site-specific persistence probabilities that vary across the species range (Peacock and Smith 1997; Jeffress et al. 2013; Castillo et al. 2014; Schwalm et al. 2016). Indeed, pika populations continue to persist in some low-elevation sites (Beever et al. 2008; Rodhouse et al. 2010; Manning and Hagar 2011; Jeffress et al. 2017), which may reflect the nuances of local habitat suitability and potential for behavioral plasticity in this species (Erb et al. 2011; Varner and Dearing 2014; Moyer-Horner et al. 2015; Mathewson et al. 2017).
This study examines changes in patch occupancy, levels of genetic diversity, and dispersion of genetic variation across the landscape for an iconic pika metapopulation in the Bodie Hills (Mono County, California) (Severaid 1955; Smith 1974; Peacock and Smith 1997), a low elevational spur of the main Sierra Nevada mountain range on the border with Nevada. Stewart et al. (2015) recently investigated climate change and pika persistence in the Sierra Nevada, which included the Bodie population, and showed that average summer temperature and talus extent within a one km radius were predictors of both current occupancy and extirpation for historically occupied sites in the Sierra Nevada. Now protected as a California State Historic Park (BSHP) (elevation, ~ 2500 m), the BSHP population is one of the only extant pika populations remaining within the Bodie Hills as almost all the natural rock outcroppings found here are currently unoccupied by pikas despite evidence of recent 20th and 21st century occupation (Nichols 2011; Stewart et al. 2015; Nichols et al. 2016).
Embedded within Great Basin sagebrush-scrub plant community, pika habitat at BSHP is composed of ore dumps created by hard-rock mining during the late 19th and early 20th centuries, and pikas are believed to have colonized these ore dumps from neighboring natural talus in the early 1900s (Fig. 1; Severaid 1955). The pika population at BSHP was first reported by J.H. Severaid (Severaid 1955) and has been under continuous study since 1969 (Smith 1974a, 1974b, 1978; Peacock and Smith 1997; Moilanen et al. 1998; Nichols 2011; Stewart et al. 2015; Nichols et al. 2016; Klingler, Jahner et al. 2021). This population has been the subject of studies on metapopulation dynamics (Peacock and Smith 1997; Moilanen et al. 1998), population genetic structure (Peacock and Smith 1997), species distribution modeling (Stewart et al. 2015) and most recently a range wide comparison of genomic variation among multiple lineages and subspecies (Klingler, Jahner et al. 2021).
We use the results of two early census periods in 1972 and 1977, together with 30 years of annual BSHP population census survey data (Moilanen et al. 1998; Nichols, this study) as well as contemporary population genetic data (1988–1991 and 2013–2015), to test the hypothesis that genetic diversity has eroded at this site due in part to changes in patch occupancy likely attributable to 20th and 21st century climate change. Furthermore, we provide historical context of the population genetic diversity once present at this site by comparing these two sets of more contemporary genetic samples to museum samples collected at BSHP in 1948 and 1949 by J.H. Severaid and curated at the Museum of Vertebrate Zoology (MVZ), University of California at Berkeley. In addition, we also provide a regional context by comparing BSHP samples to historic samples collected at Big Indian Mountain (BIH), Wassuk Range, Mineral County Nevada, ~ 35 km northeast of BSHP, by S.B. Benson and O.P. Pearson in 1947 (curated at MVZ).
Recent census data estimates the extant population to be < 100 individuals, representing about 100 pika generations since colonization from natural outcrops circa 1900. Ore dump patches that had been previously occupied and were therefore considered suitable habitat in the southern and middle sections of BSHP experienced a population collapse sometime in the 1980s which was later documented by the 1989 census (Fig. 1; Moilanen et al. 1998). The southern half of the study area has never fully recovered with only a few of the extirpated talus patches being intermittently recolonized by the extant population in the northern half of the mining district (Moilanen et al. 1998; Nichols, this study). The increasing isolation of the BSHP pika population within the Bodie Hills during recent years (Nichols et al. 2016) occurred simultaneously with severe drought (2012–2014) in California that led to increasingly warm air temperatures and low levels of precipitation (Griffin and Anchukaitis 2014; Diaz and Wahl 2015). The frequency of drought years during the last two decades has increased compared to the previous 100 years and the likelihood of extremely warm, low precipitation years is projected for the near future (AghaKouchak et al. 2014; Diffenbaugh et al. 2015; Williams et al. 2015).
We hypothesize that the warming air temperatures and decreased precipitation documented for this region have negatively affected survivorship, recruitment and patch occupancy of pikas at BSHP over the latter half of the 20th and early 21st centuries. We also hypothesize that changes in patch occupancy, in terms of both the duration of occupation and turnover dynamics, have fundamentally altered the metapopulation dynamic of this site and led to genetic coalescence and concomitant losses in genetic diversity (Gilpin 1991). Therefore, we expect to observe evidence of a disrupted metapopulation dynamic (Peacock and Smith 1997) that includes: (1) a steady reduction in the proportion of patches occupied (as measured by proportion of patches occupied/total patches surveyed), (2) evidence of genetic coalescence and genetic erosion via a decline in allelic diversity and heterozygosity, (3) a decrease in the effective population size (Ne) over the 20th and 21st centuries and (4) increasing regional isolation.