32. BALANUS HAMERI. Pl. 7, fig. 5 _a_-5 _c_.

LEPAS HAMERI. _Ascanius._ Icones rerum naturalium, Tab. 10, 1767.

---- TULIPA. _O. F. Müller._ Prodromus. Zoolog. Dan. 1776; sed non

_L. tulipa_, in Poli, Test. ut. Siciliæ; neenon _B. tulipa_, in

Bruguière, Encyclop. Method; neenon _B. tulipa_, in Sowerby,

Genera of Shells.

---- TULIPA ALBA. _Chemnitz._ Syst. Conch. Tab. 93, fig. 832.

---- FOLIACEA. _Spengler._ Skrivter of Naturhist. Selskabet, 1 B.

1790.

BALANUS CANDIDUS. (Tab. emendata) _Brown._ Conch. Great Britain

(1827), Tab. 6, figs. 9 and 10, et 2d edit. Tab. 54, figs. 9-12.

---- TULIPA. _Lyell._[98] In Phil. Transact., 1835, p. 37, Tab. 2,

figs. 34-39.

[98] Sir C. Lyell remarks that this is apparently the _B.

Uddevallensis_ (Linn.) of Swedish lists of fossils. Prof. E. Forbes

has shown (Mem. Geolog. Survey of England, vol. 1, p. 364) how this

name arose, from a short description, prior to the introduction of

the binomial system, "Lepas quæ Balanus Uddevallensis," given by

Linnæus in his Wast-Gotha Resa, in 1747.

For the reference to Ascanius' work, which is on the binomial

system, and subsequent to the 10th edit. of Linnæus, in 1758, I am

greatly indebted to Mr. Sylvanus Hanley. Had it not been for this

gentleman, I should have used Müller's name of _B. tulipa_ as the

first name.

_Shell white: radii with their oblique summits smooth and arched;

sutural edges smooth: basis solid. Scutum feebly striated

longitudinally: tergum with the spur narrow._

_Hab._--Coast of Yorkshire; Scotland; Galway, Ireland; Isle of Man,

and Anglesey, twelve fathoms. Generally in deep water; not very

common. George's Bank, Massachussetts, United States; Mus. Aug.

Gould. Iceland, Finmark, and the Faroe Island, according to Spengler.

Attached to crustacea, mollusca, stems of fuci, and stones; often

associated with _B. porcatus_ and _crenatus_.

_Fossil._--In glacial deposits at Uddevalla in Sweden, and Beaufort

in Canada; Mus. Lyell. Banks of the Dwina, Russia; Mus. Murchison.

Greenland, "in blue clay," according to Spengler. Red Crag (Sutton)

Mus. S. Wood.

_General appearance._--Shell tubulo-conical, very smooth, white,

generally more or less covered by yellow thin membrane: orifice

large, sub-triangular: radii moderately broad, with their more

or less oblique summits slightly rounded and smooth; from this

circumstance the shell has been justly compared to the half-opened

flower of a white tulip. Specimens often exceed an inch in basal

diameter; I have seen one from Scarborough two inches in diameter

and one and three quarters in height: another specimen was 1.6 in

diameter and 3 in height. The specimens in the glacial deposits seem

even to have acquired larger dimensions, one from Uddevalla being

nearly four inches in height.

_Scuta_, elongated, flat, feebly striated longitudinally:

internally, articular ridge short, moderately prominent: adductor

ridge, confluent in the upper part with the articular ridge,

running straight down and forming a rather large cavity for the

lateral depressor. _Terga_ feebly striated longitudinally, with a

longitudinal furrow, having the sides, in old specimens, partly

closed in: the basal margin slopes much towards the spur, which is

rather long and narrow, with its end rounded: it is placed at about

its own width from the basi-scutal angle. Internally, articular

furrow narrow; crests for the depressores moderately prominent, but

in a variable degree.

_Compartments_: these are unusually thin, and separate easily: the

parietes are finely ribbed longitudinally on their insides; the

bases of these ribs being just perceptibly denticulated. _Radii_,

with their summits oblique (usually at about an angle of 45°),

slightly arched and quite smooth: the smoothness is produced by the

edge being a little inflected: sutural edge quite smooth, without

even a trace of septa or denticuli. _Alæ_ oblique, generally rather

less oblique than the summits of the radii: sutural edges smooth,

with an excessively fine linear furrow running along the edge, a

little towards the inner side, and filled with a yellow ligamentous

substance: a furrow of this kind I have seen in no other species.

_Basis_, solid, not permeated by pores; either smooth, or slightly

furrowed in lines radiating from the centre.

_Mouth_: labrum with scarcely perceptible minute bead-like teeth

thinly scattered along the edge. _Palpi_ and _outer maxillæ_ rather

sparingly clothed with hairs. _Mandibles_ with teeth rather sharp;

the fourth and fifth teeth small, but well developed; inferior angle

pointed with fine spines. _Maxillæ_ with a deep notch under the two

upper great spines. _Cirri_, the first pair is short, with rami of

nearly equal length: the segments are not protuberant in front either

in the first or second pairs. In the posterior cirri, the segments

bear four pairs of spines, with a tuft of rather long intermediate

spines: in young specimens there are only three pairs: the spines in

the dorsal tufts are short and thin.

When the shell is disarticulated, this species cannot be confounded

with any other; but judging by external characters alone, it may

sometimes be very easily confounded with _B. eburneus_, and I have

received the two species under this one name from Massachussetts:

generally _B. Hameri_ may be distinguished from _B. eburneus_ by

the smoothness of the summits of its radii, and by the so-called

epidermis being of a darker yellow.

With respect to the fossil specimens from the glacial deposits,

I have little to add; I have seen one from Uddevalla, as already

remarked, four inches in height, and a lateral compartment broader by

one fourth than the same compartment in any recent specimen. As Sir

C. Lyell remarks (Phil. Transact.), the compartments are always found

separated, which is accounted for by their weak union in a recent

state. This species, when fossil, is usually associated with its

deep-water congeners _B. porcatus_ and _crenatus_, as at the present

day.

I must here mention that I have examined a considerable number of

_separated_ compartments, without opercular valves, brought from

Barbados, in the West Indies, showing the existence there of a

closely allied or possibly identical species. The only difference

which I can point out in these compartments is, that the parietes

are rather thicker, and the radii rather narrower, with more oblique

summits: some of the compartments are two inches in length. It seems

very improbable that the true _B. Hameri_ should extend to the West

Indies, but after what has been seen in the case of _B. crenatus_,

this is possible.

A Monograph on the Sub-class Cirripedia (Volume 2 of 2) The Balanidæ, (or Sessile Cirripedes); the Verrucidæ, etc., etc. · 第 78 / 417 题