One of the mysteries of the origin of animal phyla is the emergence of animals with an endoskeleton (internal skeleton). The main question is, how did such internal bones form? There is no explanation found in the fossil remains nor are there any sound theoretical models. The few known fossils of invertebrate chordates give no further clues as to the origin of vertebrates (vertebrates belong to the chordates, see Figure 188).
One must keep in mind what changes are needed in the blueprint of an animal in order to build a system of bones, vertebrae, tendons and associated muscles! These fundamental transformations would have required so many intermediate stages over such a long period of time that you should find some relevant fossils in Precambrian and Cambrian rocks. A perhaps suitable precursor to vertebrates is Pikaia (Figure 189) from the Canadian Burgess Shale (Middle Cambrian). Its body shape is reminiscent of the lancelet (Fig. 188). The animal has a striped cord along its back, which is interpreted as a notochord, and the typical zig-zag stripes of myotomes (muscle bands).
Only recently, the oldest documented vertebrate fossils were discovered. These were fossils of the jawless fish Myllokunmingia and Haikouichthys (Fig. 190) which appears in the Lower Cambrian, at the famous fossil site Chengjiang (China) and thus in strata older than where the Pikaia was found.
In general, Carroll (1993, p. 16) states of the oldest known vertebrates, that they differ so much from each other, "that their family relationships could only be reconstructed with great difficulty.” Each of these groups has a mosaic of primitive and derived features, but none approaches the anatomical characteristic pattern that one would expect for a primitive ancestor of the other groups. Evolutionary theory therefore assumed that the bones were acquired independently in several stages and in many different lines of development (convergence, see Similarities in Morphology and Anatomy). Today, due to the lack of fossils, the relationship of vertebrates to other phyla has been reconstructed based on existing life forms. |
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In the Lower Cambrian, fossil representatives of all known animal phyla), which have hard parts, occur almost simultaneously in a large variety of forms and over a wide geographical area. In comparison, the underlying Precambrian rocks contain few multicellular organisms, of which only a few could be interpreted as a precursors to Cambrian forms. The sudden appearance of so many different blueprints (different phyla) at the beginning of the fossil record is also an enigma for evolutionary biologists. |