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A Generic Revision and Phylogenetic Analysis of the Primnoidae

A Generic Revision and Phylogenetic Analysis of the Primnoidae

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smooth state transforms to granular (state 1) from which<br />

<strong>the</strong> spiny (state 4), nodular (state 3), ridged (state 2), <strong>and</strong><br />

tuberculate ridge (state 6) states evolved; however, <strong>the</strong>re is<br />

rampant homoplasy among <strong>the</strong>se character states, resulting<br />

in a low CI (0.429). None<strong>the</strong>less, at least one <strong>of</strong> <strong>the</strong><br />

transitions to <strong>the</strong> ascus scale morphology helps to defi ne<br />

clade C″, <strong>the</strong> Fannyella-type genera.<br />

Character 22 (Infrabasals). The state<br />

<strong>of</strong> <strong>the</strong> out-group <strong>and</strong> most primnoid taxa, including <strong>the</strong><br />

ancestral state, is to lack infrabasal scales (state 0). But<br />

within clade D (Calyptrophorinae) <strong>the</strong>re is a progression<br />

from none (state 0) to one pair (state 1) to more than one<br />

pair (state 2), which gives some resolution within this<br />

clade. The CI is 1 for this character.<br />

Character 23 (Number <strong>of</strong> Coenenchymal<br />

Layers). The ancestral state as well as that<br />

<strong>of</strong> <strong>the</strong> out-group is to have two layers <strong>of</strong> sclerites (state<br />

0), as suggested by Versluys (1906). Although <strong>the</strong> CI for<br />

this character is low, it does serve to distinguish <strong>the</strong> two<br />

largest clades within <strong>the</strong> family (clades B <strong>and</strong> C) <strong>and</strong> is still<br />

considered to be signifi cant.<br />

Characters 2, 14, <strong>and</strong> 20 are autapomorphic <strong>and</strong> thus<br />

do not contribute to tree topology. Likewise, characters<br />

24–27 were included to show how <strong>the</strong> <strong>Primnoidae</strong> differ<br />

from <strong>the</strong> out-group <strong>and</strong> thus show evidence <strong>of</strong> <strong>the</strong> monophyly<br />

<strong>of</strong> <strong>the</strong> <strong>Primnoidae</strong>. They do not contribute to tree<br />

structure.<br />

In summary, <strong>the</strong> characters that show high CI <strong>and</strong>/or<br />

signifi cant support for clades are 8 (presence or absence<br />

<strong>of</strong> an operculum), 10 (correspondence <strong>of</strong> marginal <strong>and</strong><br />

opercular scales), 16 (<strong>the</strong> number <strong>of</strong> longitudinal body<br />

wall scales), 18 (<strong>the</strong> number <strong>of</strong> adaxial rows <strong>of</strong> body wall<br />

scales), <strong>and</strong> 19 (<strong>the</strong> number <strong>of</strong> scales in each body wall<br />

row). Characters <strong>of</strong> little value in illustrating generic affi<br />

nities include 1 (colony shape), 4 (basal fusion <strong>of</strong> calyces),<br />

6 (proximity <strong>of</strong> calyces to stem), 13 (distal margin <strong>of</strong><br />

marginal scales), <strong>and</strong> 21 (external sculpture <strong>of</strong> body wall<br />

scales).<br />

SYSTEMATIC ACCOUNT<br />

SUBCLASS OCTOCORALLIA<br />

ORDER GORGONACEA<br />

number 629 19<br />

SUBORDER CALCAXONIA GRASSHOFF, 1999<br />

FAMILY PRIMNOIDAE MILNE EDWARDS, 1857<br />

Diagnosis. Cross section <strong>of</strong> axis reveals undulating<br />

concentric layers <strong>of</strong> calcifi ed material embedded in<br />

gorgonin, resulting from a longitudinal (not radial) pattern<br />

<strong>of</strong> calcifi cation (Bayer, 1955:pls. 4e–f). This arrangement<br />

usually results in a longitudinally striate (or grooved)<br />

outer axial surface; axis solid <strong>and</strong> continuous (with only<br />

one exception, Mirostenella, which has a jointed axis),<br />

without a chambered central core. Colonies branched in a<br />

variety <strong>of</strong> manners or unbranched, usually fi rmly attached<br />

to substrate by a calcareous discoidal holdfast. Polyps<br />

nonretractile, <strong>the</strong> calyces occurring in a variety <strong>of</strong> arrangements<br />

<strong>and</strong> orientations, in one case (Ainigmaptilon) arranged<br />

in clusters on leaf-like structures. Polyps heavily<br />

armored with calcareous scales that are usually arranged<br />

in an imbricate manner: each calyx has eight triangular<br />

opercular scales forming a closeable operculum, a variable<br />

number <strong>of</strong> marginal (also called buccal or circumopercular)<br />

scales (usually eight), <strong>and</strong> a variable number <strong>of</strong> rows<br />

<strong>of</strong> longitudinal body wall scales (<strong>of</strong>ten eight). Scales distinguished<br />

by <strong>the</strong> cruciform extinction pattern (Figure 3c),<br />

revealed in polarized light (dark fi eld or crossed Nicol fi lter),<br />

that results from a radial crystal orientation (Bayer,<br />

1956:F221, fi g. 158-5). Coenenchymal sclerites also predominantly<br />

imbricate scales, but some genera also have<br />

an inner layer <strong>of</strong> tuberculate spheroids that compose <strong>the</strong><br />

walls <strong>of</strong> <strong>the</strong> longitudinal canals.<br />

Type genus. Primnoa Lamouroux, 1812.<br />

Distribution. Worldwide (especially common<br />

in Antarctic region), occurring predominantly at<br />

slope depths, but ranging from 8 to 5,850 m.<br />

ARTIFICIAL INDENTED KEY TO THE GENERA OF PRIMNOIDAE<br />

I. Polyps united in groups forming polyp leaves [Figure 4p] placed along axis as in some pennatulaceans: “Subfamily<br />

Ainigmaptilinae”: Ainigmaptilon<br />

II. Polyps individually distinct or united basally [Figure 3i], but not united in groups forming polyp leaves: “Subfamily<br />

Primnoinae”<br />

A. Polyps adnate [Figure 4b] to coenenchyme except for oral region.<br />

1. Colonies dichotomous, large, <strong>and</strong> robust, terminal branches long <strong>and</strong> fl exible; polyps large, arranged in closeset<br />

whorls, abaxial side covered by two rows [Figure 4a] <strong>of</strong> narrow, sickle-blade-shaped sclerites [Figure 4e];<br />

distalmost polyp scales not differentiated as operculum [Figure 4b]: Armadillogorgia

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