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Zoogeography<br />

I. Northeastern Pacific<br />

A. Tropical (PANAMANIAN PROVINCE, including "CORTEZ PROV-<br />

INCE")<br />

B. Temperate Region<br />

1. Warm Temperate (CALIFORNIA PROVINCE, including "SAN<br />

DIEGO PROVINCE")<br />

2. Cold Temperate<br />

a. Lower Boreal (OREGON PROVINCE)<br />

b. Upper Boreal (ALEUTIAN PROVINCE)<br />

II. Northwestern Pacific<br />

A. Tropical (INDO-WEST PACIFIC PROVINCE)<br />

B. Temperate Region<br />

1. Warm Temperate (JAPAN PROVINCE)<br />

2. Cold Temperate<br />

a. Lower Boreal (ORIENTAL PROVINCE)<br />

b. Upper Boreal (KURILE and OKHOTSK PROVINCES)<br />

TEMPERATE NORTHEASTERN PACIFIC.—In general, the<br />

boundaries of the various zoogeographic regions and provinces<br />

discussed in this analysis follow the synthesis of Briggs (1974,<br />

see outline above); however, an exception was made with<br />

respect to the southern boundary of the warm termperate<br />

province of the northeastern Pacific. Briggs recognized a<br />

distinct warm temperate province, called the Cortez Province,<br />

1 halfsystem<br />

Pourtales Plan<br />

system<br />

FIGURE 2.—Composite cross-sectional diagram of a calice illustrating various<br />

septal insertion patterns: upper right system with three cycles of septa, upper<br />

left system with four cycles, and lower two systems with various stages of<br />

development of the Pourtales Plan (after Cairns and Parker, 1992). Numbers<br />

refer to cycle to which septa belong.<br />

SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY<br />

TABLE 3.—Azooxanthellate Scleractinia known from the Gulf of California<br />

Aslrangia haimei Verrill, 1866<br />

Astrangia coslata Verrill, 1866<br />

Astrangia conferia Verrill, 1870a<br />

Paracyathus stearnsii Verrill, 1869<br />

Coenocyalhus bowersi Vaughan, 1906<br />

Ceratotrochus franciscanus Durham and Barnard, 1952<br />

Phyllangia consagensis (Durham and Barnard, 1952)<br />

Desmophyllum dianthus (Esper, 1794)<br />

Balanophyllia cedrosensis Durham, 1947<br />

Endopachys grayi Milne Edwards and Haime, 1848b<br />

Dendrophyllia oldroydae Oldroyd, 1924<br />

Tubastraea coccinea Lesson, 1829<br />

that included the waters of the Gulf of California from La Paz,<br />

Baja California on the west coast of the Gulf to Topolobampo,<br />

Sinaloa, Mexico on the eastern coast. However, most zoogeographers<br />

(e.g., Ekman, 1953; Squires, 1959; Brusca, 1980)<br />

consider the Gulf of California to be an attenuated tropical or<br />

subtropical fauna. This categorization is supported by the<br />

affinities of the 12 azooxanthellate species found in the Gulf<br />

(Table 3). Aside from three species that are cosmopolitan,<br />

seven of the remaining nine species known from the Gulf are<br />

tropical species with their northern limits in the Gulf, or<br />

eurythermic tropical species having their northern limits<br />

slightly farther north in the warm temperate region. Only one<br />

species, Paracyathus stearnsii, is primarily temperate in<br />

distribution, and one species, Ceratotrochus franciscanus, is<br />

endemic to the Gulf. The endemic nature of the latter species<br />

must be viewed with doubt because it is known from only one<br />

specimen.<br />

The northern boundary of the northeastern Pacific warm<br />

temperate California Province is generally regarded as Point<br />

Conception, California, but its southern boundary on the<br />

Pacific coast of Baja California is less well defined. Various<br />

zoogeographers have placed it as far south as Cabo San Lucas<br />

and as far north as Bahia Sebastian Vizcaino (see Briggs,<br />

1974); however, the latitude of Isla Magdalena (24°40'N) is<br />

most often cited, and is adopted in this analysis. At least one<br />

tropical azooxanthellate, Astrangia conferta, has its northern<br />

limit at Isla Magdalena, and this latitude also coincides with the<br />

northern limit of zooxanthellate corals on the northeastern<br />

Pacific coast of Baja California (Squires, 1959; Wilson, 1988,<br />

1991). Seventeen scleractinians are known to occur in the<br />

California Province (Table 4), of which four are cosmopolitan<br />

and one, Crispatotrochusfoxi, has a disjunct distribution in that<br />

province and the Aleutian Province. Two species are endemic<br />

to the province (Nomlandia calif or nica and Dendrophyllia<br />

californica), but both of these are known from very few records.<br />

One species, Leptopenus discus, appears to be bitemperate,<br />

occurring in the northern and southern temperate regions. The<br />

remaining nine species are an almost equal mixture of five<br />

eurythermic tropical species and 4 eurythermic temperate<br />

species, consistent with Briggs' (1974) characterization of this<br />

province as a transition zone between the tropical and<br />

temperate regions. Rocas Alijos, a small group of rocks 343 km<br />

west of Isla MagdaJena at 24°57'N, was included in the warm

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