Jw. Sites et al., PARAPATRIC HYBRIDIZATION BETWEEN CHROMOSOME RACES OF THE SCELOPORUS-GRAMMICUS COMPLEX (PHRYNOSOMATIDAE) - STRUCTURE OF THE TULANCINGO TRANSECT, Copeia, (2), 1993, pp. 373-398
Genetic and morphological studies were carried out on a total sample o
f 108 individuals of the Sceloporus grammicus complex, collected from
eight sites along a transect in eastern Hidalgo, Mexico. Samples were
collected from both sides and through the middle of a zone of parapatr
ic hybridization between F5 (2n = 34) and FM2 (2n = 46) chromosome rac
es of this group to assess general patterns of gene flow across the zo
ne for independent sets of markers. Karyotypic and morphological data
were collected from almost all lizards; and allozyme, mitochondrial-DN
A and ribosomal-DNA restriction site data were collected from a subset
of the total. Three unambiguous diagnostic chromosome markers defined
the zone by showing sharp, concordant changes from one parental race
to the other over a distance of about 2 km. Virtually no introgression
of any of these markers occurred outside of localities immediately ad
jacent to the point of contact, and this transition was also reflected
in diagnostic classes of mtDNA haplotypes, albeit slightly asymmetric
al in the direction of F5 introgression. Ribosomal-DNA genotypes intro
gressed more extensively in both directions. No fixed genic difference
s were found between these cytotypes in a sample of 42 loci, but alloz
yme frequencies in five polymorphic loci displayed frequency shifts ac
ross the transect, as did the distribution of mtDNA haplotypes. Morpho
logically, chromosomally pure individuals in the zone could be correct
ly assigned to their appropriate parental populations outside of the z
one with a high degree of confidence. F1 and backcross individuals wer
e morphologically intermediate in multivariate analyses, although they
overlapped with both groups of parental phenotypes, and very few sing
le traits displayed intermediacy. The structure and shape of the diagn
ostic character clines are discussed with respect to the origin and ma
intenance of this zone.