No. 27: May-Jun 1983
Just offshore of Guadeloupe, in the West Indies, lies a kilometer-long formation of extremely hard limestone dated as Miocene, or about 25 million years old. Nothing surprising so far! However, history records that in the late 1700s many human skeletons -- all indistinguishable from modern humans -- were excavated from this limestone. One of the quarried specimens, ensconced in a 2-ton slab, was shipped to the British Museum. It arrived in 1812 and was placed on public display. With the ascendance of Darwinism, the fossil skeleton was quietly spirited away to the basement.
The discovery of these human remains has been well-documented in the scientific literature. Here is another pertinent geological fact: the limestone formation in question is situated 2-3 meters below a 1-million-year-old coral reef.
If the limestone is truly 25 million years old, the human evolutionary timetable is grossly in error. Even if this is not the case, and the bones are merely 1 million years old or so, as required by the coral reef; then, fully modern humans lived in the New World long before the Bering Land Bridge went into service. The only way a serious geological or archeological anomaly can be avoided is to predicate that the limestone formation was really laid down in the last 10,000-20,000 years -- something like that doesn't seem too likely.
(Cooper, Bill; "Human Fossils from Noah's Flood," Ex Nihilo, 1:6, no. 3, 1983.)
Comment. This sort of dating puzzle is manna to the scientific creationists. It is therefore not surprising to discover that Ex Nihilo is published by the Creation Science Foundation of Australia. Nevertheless, the Guadeloupe skeletons truly exist -- it's just that the creationists seem to be the only ones talking about them. You have seen their slant on them above. Other interpretations of the Guadeloupe skeletons will be presented in future issues.
Reference. Additional information on the Guadeloupe skeleton may be found at BHE12 in our Catalog: Biological Anomalies: Humans III. For details, visit: here.
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