Dendrocystoides
scoticus
Deuterostomata,
Class Homalozoa, Order Soluta
Geological
Time: Upper Ordovician, Ashgillian Stage Size (25.4
mm = 1 inch): Theca: 15 mm by 21 mm with 9 mm feeding tube and 33 mm
articulated
stem Matrix: 80 mm by 60 mm
Fossil Site:
Lady Burn Starfish Beds, Girvan District, Ayrshire, Scotland
Code: UKF153
Price: Sold
Description:
I have recently been able to acquire a number of specimens coming
from the famous Upper Ordovician Lady Burn Starfish Beds of the
Girvan District of Scotland. While it is the most important starfish
locality in the British Isles, it also contains a diverse representation
of trilobites, crinoids, carpoids and others. Specimens from
the locality are not often made available, so this diverse grouping
is most uncommon. This plate contains an excellent example of
the carpoid Dendrocystoides scoticus. The species name derivation
is obvious. The carpoids are one of the most contentious groups
of fossil organisms known. While they have been studied for over
150 years, their unique character combinations have caused a
number of disputes over both their paleobiology and relationships.
While some place them in the Echinodermata, their lack of pentaradial
symmetry calls that placement into question. Additionally many
carpoids are thought to have possessed gill slits, a feature
characteristic of chordates and hemichaordates. Many possess
one or two “appendages” which have been interpreted
variously as feeding tubes, tails with notocords and muscular
feet. The carpoid body was supported by a skeleton of calcitic
plates like those found in modern Echinoderms. Some believe that
a carpoid may have been the common ancestor between Echinoderms
and Vertebrates. It is important to note the carpoids differ
from ALL other animals, living and extinct, in that many are
completely asymmetrical. With so much debate over assignment
of the appendages to specific functions, how can one come to
a conclusion about their assignment in the Tree of Life?.
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