(cross-section); from:
Charles Lyell (1863):
The Geological Evidences of the Antiquity of Man. Limestone has been mined in the Neander Valley since the early 16th century. By the mid-19th century, mining operations had expanded to an industrial scale. In August 1856, two Italian workers extended the entrance to the
Kleine Feldhofer Grotte by removing the naturally
sintered, rock-hard clay layers embedded in the limestone of the cave. During the removal of the sediment fillings, the workers unearthed fossilized bones at a depth of . Initially unnoticed, the bones were discarded among the mud and debris and scattered throughout the valley. The discovery came to the attention of the cave's owner, Wilhelm Beckershoff, who assumed the bones belonged to a
cave bear. Beckershoff, along with quarry co-owner Friedrich Wilhelm Pieper, retrieved 16 bones and fragments from the rubble and handed them to
Elberfeld teacher and fossil collector
Johann Carl Fuhlrott. Among the preserved remains were a
skullcap with a fragment of the left
temporal bone, a fragment of the right
scapula, a right
clavicle, both
humeri (with the right side intact), a complete right
radius, fragments of the right and left forearm bones, five ribs, an almost complete left half of the
pelvis, and both
femora. Fuhlrott reportedly recognized immediately that the remains belonged to a human who significantly differed from modern humans. Without his consent, a notice was published on September 4, 1856, in the
Elberfeld newspaper and the Barmer Local Journal: In neighboring Neanderthal, a surprising discovery was made in recent days. The removal of the limestone rocks, which certainly is a dreadful deed from a picturesque point of view, revealed a cave that had been filled with mud-clay over the centuries. While clearing away this clay, a human skeleton was found. Undoubtedly, it would have been ignored and lost if not for the timely intervention of Dr. Fuhlrott of Elberfeld, who secured and examined the find. Examination of the skeleton, particularly the skull, suggests it belonged to the tribe of the Flat Heads, which still exists in the American West and of which several skulls have been found in recent years on the upper
Danube in
Sigmaringen. Perhaps this find can help determine whether the skeleton belonged to an early central European native or simply to one of
Attila's roaming horde. This report drew the attention of two
Bonn professors of anatomy,
Hermann Schaaffhausen and August Franz Josef Karl Mayer. They contacted Fuhlrott and requested to examine the bones. Fuhlrott personally brought the remains to Bonn during the winter, where Schaaffhausen conducted an investigation. On June 2, 1857, Schaaffhausen and Fuhlrott presented their findings to the members of the
Natural History Society of the Prussian Rhineland and Westphalia. Paleoanthropologist
Ian Tattersall summarized their findings: Here, Fuhlrott summarized the history of the discovery, based on a careful survey of the workers who had excavated the finds. He emphasized the age of the bones, evident from the thickness of the overlying strata [...] as well as from the strong
mineralization and
dendrite formation on the surface, also present in the bones of extinct giant cave bears. Schaaffhausen described and interpreted the find. Schaaffhausen noted the unusually massive bone structure, particularly the cranium’s low, sloping forehead and prominent brow ridges: He considered these characteristics natural rather than pathological or the result of abnormal development. These traits reminded him of the
great apes. However, this was not an ape. If the features were not pathological, they must have been due to the age of the remains. [...] Although Schaaffhausen's own search for comparable specimens was unsuccessful, he concluded that the bones belonged to a native tribe that had inhabited Germany before the arrival of modern humans. Schaaffhausen published his findings in 1858 in the
Archives of Anatomy, Physiology, and Scientific Medicine. A year later, Fuhlrott published a
Treatise on Human Remains from a Rock Grotto of the Düssel Valley in the journal of the
Natural History Society of the Prussian Rhineland and Westphalia. In this essay, Fuhlrott cautiously suggested that the bones likely originated from "prehistoric times, probably from the diluvial period, and therefore belonged to an archetypal individual of our race." Reflecting on the geological context, he speculated that the remains might be "ante-diluvial" (pre-dating the
biblical flood), representing fossilized humans. Fuhlrott’s and Schaaffhausen’s interpretations, although ultimately correct, were not initially taken seriously by many scholars. When Fuhlrott published his treatise in 1859, the editorial committee of the
Natural History Society of the Prussian Rhineland and Westphalia added a dismissive postscript, noting that he had "put forward views that cannot be shared." ==Historical background==