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The Spirit in Human Evolution - Waldorf Research Institute

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Paleolithic cultures. At High Lodge <strong>in</strong> East Anglia, England, now reliably dated to<br />

around 500,000 BP, stone artifacts have been found which stylistically belong to Middle<br />

Paleolithic types. Most unusually, there is an absence of that archetypal Lower Paleolithic<br />

artefact, the Acheulian hand-axe. At Boxgrove <strong>in</strong> Sussex, which has been dated to around<br />

0.5 mya, hand-axes were found, confirm<strong>in</strong>g its status as a Lower Paleolithic site, but the<br />

axes are of such quality that without the reliable dat<strong>in</strong>g of the site they would have been<br />

considered as belong<strong>in</strong>g to a much later date. 12<br />

On the other hand, crude tools <strong>in</strong>clud<strong>in</strong>g simple hand-axes, core and flake tools<br />

have been found at Pontnewydd <strong>in</strong> Wales, dated at around 200,000 BP. <strong>The</strong>ir appearance<br />

would otherwise suggest a much earlier date. This paradox of early “advanced”<br />

forms and late “crude” forms occurs at one site, Swanscombe, <strong>in</strong> the Thames Valley.<br />

A lower level dated to between 420,000 and 360,000 BP conta<strong>in</strong>ed no hand-axes, but a<br />

comprehensive collection of Clactonian flake tools. Above these at a subsequent level<br />

is an almost classical assemblage of beautifully made Acheulian hand-axes and other<br />

typically Lower Paleolithic artifacts. Both levels are older than Pontnewydd.<br />

To compound matters, the cliff-foot site at La Cotte on Jersey, dated to around<br />

238,000 BP, revealed a dom<strong>in</strong>ance of flake tools, notably show<strong>in</strong>g the Levallois technique,<br />

usually associated with the Middle and Upper Paleolithic. <strong>The</strong> site at Ehr<strong>in</strong>gsdorf <strong>in</strong><br />

Eastern Germany also shows an absence of hand-axes and a predom<strong>in</strong>ance of ref<strong>in</strong>ed<br />

flake tools, long thought to be late-Neanderthal, but now dated much earlier to 225,000<br />

BP. Vértesszöllös <strong>in</strong> Hungary is another “early” culture with a surpris<strong>in</strong>gly “late” date.<br />

Here pebble tools of the early Lower Paleolithic style, crude <strong>in</strong> comparison to Acheulian<br />

hand-axes and Levallois technique, turn out to belong to a period between 210,000 and<br />

160,000 BP! <strong>The</strong>se examples, and similar ones cited below <strong>in</strong> the context of the appearance<br />

of Upper Paleolithic <strong>in</strong>dustries at “early” dates, highlight the follow<strong>in</strong>g po<strong>in</strong>ts.<br />

Firstly, they highlight the limitations of assum<strong>in</strong>g a l<strong>in</strong>ear ascent of technological<br />

progress proceed<strong>in</strong>g from simple to complex, from primitive to advanced. Secondly,<br />

they <strong>in</strong>troduce the concept of localized developments appear<strong>in</strong>g and then apparently<br />

disappear<strong>in</strong>g, developments which did not necessarily pass on their achievements to the<br />

“cultural gene pool” of mank<strong>in</strong>d <strong>in</strong> any material way.<br />

At any rate, these and other aspects of archeology discussed below, certa<strong>in</strong>ly<br />

identify a divergence between anatomical and cultural developments and may be seen<br />

as a further symptomatic expression of the heterochromous nature of evolution which<br />

is itself a signature of the process of emancipation.<br />

More Climate Change<br />

To return to the question of climatic fluctuation, I will focus on the major changes<br />

that affected the period beg<strong>in</strong>n<strong>in</strong>g around 250,000 BP and which saw a progressive<br />

cool<strong>in</strong>g of global temperatures. This period was ma<strong>in</strong>ly temperate or cool with some brief<br />

glacial phases. It saw the emergence of the Neanderthals <strong>in</strong> Eurasia and other regional<br />

groups of Ancients <strong>in</strong> Africa and Ch<strong>in</strong>a. This was followed by a full glacial (with milder<br />

<strong>in</strong>tervals) which lasted from around 180,000 to 130,000 BP. In Africa this period saw the<br />

probable emergence of early Moderns, whilst Neanderthals consolidated themselves <strong>in</strong><br />

Eurasia, Mabas (Ancients) likewise <strong>in</strong> Ch<strong>in</strong>a, and late erectus cont<strong>in</strong>ued <strong>in</strong> Indonesia.<br />

From 130,000 to 115,000 BP warmer <strong>in</strong>terglacial conditions were widespread.<br />

_________________________<br />

12<br />

<strong>The</strong> details cited <strong>in</strong> what follows are drawn from a variety of sources <strong>in</strong>clud<strong>in</strong>g Str<strong>in</strong>ger and<br />

Gamble, 1993, Tr<strong>in</strong>kaus and Shipman, 1993, and Gamble, 1993 and 1994.<br />

227

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