Researches on the Visual Organs of the TrilobitesLindström, Gustaf
Science
Researches on the Visual Organs of the Trilobites
Lindström, Gustaf
Trilobites
This large division embraces the second and third groups or, with a
few exceptions, all the rest of the Cambrian trilobites on account of
a feature in the cephalic sculpture common to them all, though widely
different as to its first origin in both. What forms the prominent
and common characteristic of these two groups is the presence of the
_facial ridge_, which emanates from the basis or the front of the
foremost segment of the glabella and in a great variety of different
shapes continues backwards near to the posterior border of the
head. It has received several names as _eye-line, palpebral lobe,
ocular ridge, eye-lobe, ocular fillet_ (MATTHEW). In German it is
named _Augen-leiste_, in French _filet_ (BARRANDE) and in Swedish
_ögonlist_.[4] Some authors make a difference between the more narrow
part, calling it eye line, and the thicker posterior node, which they
name the palpebral lobe proper.
[Footnote 4: That name is the most current amongst the swedish authors,
together with »_palpebrallob_»; HOLM says _ögonlob_ and _frontallob_.]
As this peculiar ridge exists before any facial suture has made its
appearance and separated the head shield in five parts, viz. the median
glabellar part, the two fixed cheeks and the two free cheeks, and
as it occurs in genera which never possessed any facial suture, and
where no eye ever was formed, it is not adequate to call it an ocular
ridge etc. the more so, as it, at least during a long series of genera
succeeding each other, has had no connection whatever with any eye. I
therefore propose to call it _facial ridge_ (in swedish _faciallist_).
It occurs on the head of almost all Cambrian trilobites, excepting
the archaic ones, and it is retained in the later Cambrian Peltura,
Sphærophthalmus etc., which have real, compound eyes, as well as in a
few Lower Silurian genera as Triarthrus, Pliomera,[5] Euloma, in the
Upper Silurian Arethusina and Acidaspis and most persisting in Harpes,
ranging from the Lower Silurian Lower Red Orthoceratite Limestone into
the middle Devonian beds.
[Footnote 5: Pl. Törnquisti HOLM.]
It presents itself in the most variable shapes, and as it in fact can
be followed through its development in the oldest known species, it is
suitable to begin its description together with the characteristics
peculiar to the oldest or second group in this large subdivision, that
of the _Olenellidæ_.
=Group 1. The Olenellidæ.=
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