II - About Salticidae
Biological background of taxonomic decisions
Provisional classification of genera and subfamilies of Salticidae
The natural classification of more than 6,000 species of Salticidae has great importance in synthesizing information on these spiders and developing ways of species identification, all over the globe. The search for a concensus for delimiting the subfamilies has been ongoing for over 100 years, but a significant break through seems to occurred only now, with the new technique of gene sequencing (Maddison & Hedin, 2003, Maddison & Zhang, 2006, Maddison, Zhang & Needham, 2007, Maddison, Bodner & Needham, 2008), which has produced a phylogenetic tree proposing relationships between various taxa. The summary of major clades distribution over continents and remarks on the problems of Salticidae classification, given in the latter papers of 2003 and 2008 (see copies below) are particularly enlighting and instructive.

Inadequacies of Simon’s methodology were demonstrated by Prószyński,
1972 (see diagram above), who proposed an entirely different
approach, concentrating on standardized drawings of palps and internal structures
of epigynes. That approach has failed to produce a usable phylogeny of the
family, as often happens with one-sided analyses, but created extensive genitalic
taxonomic data (Prószyński 1966,
1968a, 1968b, 1968c, 1976, 1984a, 1984b, 19843c, 1985a, 1987 and remaining
papers by Prószyński). Diagnostic genitalic drawings
were also
used by Galiano (all papers from 1957 untill 2001) and became standard
taxonomic documentation in the world’s Salticidae literature. Documentation
of palps and epigynes (although usually not the internal structure of the epigyne)
were used regularly for defining species in a number of papers, beginning
from Peckham & Peckham
(1883-1909), Kulczyński (1884-1911),
and for selected species in numerous papers during the twentieth century,
often diagrammatized and often of little value. However, these were not used
for defining phylogenetic relationships.
Disclaimer. Names of categories above the genus level in the "Search
a taxon" display are not intended as proposals for taxa – but
serve as provisional intermediary links between genera, subfamilies,
groups of subfamilies and infra-families, necessary for the
correct functioning of the display. The database requires that no field be
left blank, so I had to invent provisional and informal interconnecting names
for the fields lacking formal names, some of these are marked by endings -es,
-s. I do not consider the usage of such interconnecting names
in this database as a formal proposal to create them, in a sense of the ICZN,
and stipulate that they will be replaced in the future by formally described
names. J. Prószyński, 2011.Some
additions
Grupa Diolenieae Simon was raised to subfamily by Gardzinska J. 2004 [ Rewizja
taksonomiczna grupy Dioleniae (Araneae: Salticidae). PhD Thesis in Akademia Podlaska,
Siedlce 1-162, illustrations plates 1-77]. Some parts of that paper were published
in Gardzinska J. 2006 [ A revision of the spider genus Ohilimia Strand, 1911
(Araneae: Salticidae). Annales zoologici, Warszawa 56(2): 375-385, illustrations
1-48], Gardzinska J., Zabka M. 2005. [A revision of the spider genus Chalcolecta
Simon 1884 (Araneae: Salticidae). Annales zoologici, Warszawa 55: 437-448, illustrations
1-59] and Gardzinska J., Zabka M. 2006 [ A revision of the spider genus Diolenius
Thorell, 1870 (Araneae: Salticidae). Annales zoologici, Warszawa 56(2): 387-433,
illustrations 1-217].
Interpretation of geographical distribution and phyletic relationships(the chapter under construction)
Faunal study of Salticidae of
Europe, gives little material to phyletic considerations, due to non-homogenous
contents of not related post-glacial immigrants, and less numerous pre-glacial
survivors. Traces of evolution are better visible in geographical areas
with
long history of environments, especially located in warm climate, and diversified,
but numerous dispersion barriers (physical, ecological, etc.). Speciation
processes were particularly intensive in centers of origin, and centers
of secondary dispersion – such as mountains in tropical climate and
islands archipelagoes. Species spread from centers into neighboring
areas, with intensity differentiated by ecological valence of species:
some spread only over small areas, other dispersed over large distances,
many died with time.
The above is the general picture I have formed for myself from general theories
of species and dynamic zoogeography. To that I added preliminary
conclusions from taxonomic studies I carried in 1960ties-1980ties on particular genera (Sitticus, Yllenus, Phintella, Pseudicius, Telamonia, and other).
The sketches below are hypotheses, which I will not be able
to develop further.

An example of hypothesis explaining origin of geographical ranges of three congeneric, but not directly sibling, species of Evarcha, is presented on the diagram below. .

Interesting result of faunal studies is possibility of deciphering history of a genus from its present day geographical distribution, correlated with morphological hints of affinities. Lack of parameter of time could be compensated to some extent by comparison of faunae of environments of known age. However, such interpretations are limited to certain span of time and the picture of history could change diametrally with new data. An example of such change begins with summary of taxonomic revisions of Sitticus (Prószyński 1983), allowing hypothesis that the genus has apparently developed in the Palaearctics, sending immigrants to North America several times: at the relatively earliest period (resemblance of the relict S. longipes to S. absolutus), during existence of Bering land bridge (S. ranieri), in the XIXth-XXth century, and precisely dated arrival of S. niveosignatus in 1958. There were also some returns back of American species into Palaearctics (S. cutleri). Origin of S. rupicola could be related to one of interglacial episodes. That nice picture has been turned upside down by phyletic studies (Maddison, Hedin, 2003) placing, Sitticus inside Neotropical group of subfamilies Amycoida. So it could be understood now that Sitticus originated in S America, dispersed to North America, some species migrated futher to Palaearctics, as testified by relict S. longipes. The remaining part of hypothesis – further development in Palaearctics and several migrations to N America could be accepted, at least for the time being.

Prószyński,
2011.