22.06.2013 Views

A Monograph of the Lichen Genus Parmelina Hale - Smithsonian ...

A Monograph of the Lichen Genus Parmelina Hale - Smithsonian ...

A Monograph of the Lichen Genus Parmelina Hale - Smithsonian ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

NUMBER 33<br />

FIGURE 8.-Number <strong>of</strong> species in section Myeloclztm in each major geographical division.<br />

linae have been collected on <strong>the</strong> Pacific Islands ex-<br />

cept for P. cl~irttlenta at higher elevations in Ha-<br />

waii. The total Old World flora (Africa, Asia, and<br />

Australia-New Zealantl) comprises 26 species.<br />

One distrihution pattern <strong>of</strong> considerable phyto-<br />

geographic interest stands out. The species <strong>of</strong> sec-<br />

tion Myeloch ma, a ra<strong>the</strong>r homogeneous group, are<br />

concentrated in India and eastern Asia (Figure 8)<br />

and only one <strong>of</strong> <strong>the</strong>m, P. aurulentn, occurs in all<br />

geographic areas (Figure 10). The species in section<br />

Pasmelina, on <strong>the</strong> o<strong>the</strong>r hand, are not strongly<br />

Concentrated in any region.<br />

TVithin section Myelochl-oa <strong>the</strong> species related to<br />

P. galbina form a particularly interesting group. As<br />

pointed out by Kurokawa (1972), P. galbina, <strong>the</strong><br />

fertile progenitor species, behaves as an Arcto-<br />

tertiary plant which migrated southward and has<br />

survived in Japan and eastern Korth America. A<br />

rare sorediate morph, P. metawvoluta, has <strong>the</strong><br />

same range, whereas <strong>the</strong> isidiate morph, P. ob.tessa,<br />

is restricted to North America, and <strong>the</strong> pustulate<br />

morph, P. hayachinensis, to Japan. W. Culberson<br />

(1972) also regards P. aimilenla as a Tertiary relict.<br />

Pai.melina has several complex groups <strong>of</strong> species<br />

that have evidently resulted from combined chem-<br />

ical and morphological evolution. The species in<br />

section iMyelochroa, for example, all <strong>of</strong> which con-<br />

tain terpenes and almost always have secalonic<br />

acid A, a yellow pigment, have evolved from two<br />

chemically dissimilar ancestors, one, <strong>the</strong> smaller<br />

group, with leucotylic acid and resembling P. ir-<br />

g.iigans, and <strong>the</strong> o<strong>the</strong>r, a larger series with leuco-<br />

tylin, resembling <strong>the</strong> present-day P. subazirzilenfa.<br />

The numerous morplis derived from <strong>the</strong>se presump-<br />

tive parents or <strong>the</strong>ir ancestors, P. nmagiensis, P.<br />

aiti.itlenta, P. crassata, P. clegelii, P. denegnns, P.<br />

ento<strong>the</strong>iochroa, P. leucotyliza, P. perisidians, P.<br />

Thytidodes, and P. xnntholcpis, have diversified<br />

mostly by production <strong>of</strong> soretlia, isidia, pustules,<br />

and wrinkles, variation in apotliecial diameter, etc.<br />

AIorph forniation (see <strong>Hale</strong>, 1975a:13) is not<br />

strongly delineated for <strong>the</strong> most part since <strong>the</strong> par-<br />

ents cannot be traced directly. \Ve are left to con-<br />

clude that section Alyelochron is an ancient group<br />

13

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!