Royal Academy of Sciences New Zealand Open Science
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‘Neanderthal bone flutes’: simply products of Ice Age spotted hyena scavenging activities on cave bear cubs in European cave bear dens

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Punctured extinct cave bear femora were misidentified in southeastern Europe (Hungary/Slovenia) as ‘Palaeolithic bone flutes’ and the ‘oldest Neanderthal instruments’. These are not instruments, nor human made, but products of the most important cave bear scavengers of Europe, hyenas. Late Middle to Late Pleistocene (Mousterian to Gravettian) Ice Age spotted hyenas of Europe occupied mainly cave entrances as dens (communal/cub raising den types), but went deeper for scavenging into cave bear dens, or used in a few cases branches/diagonal shafts (i.e. prey storage den type). In most of those dens, about 20% of adult to 80% of bear cub remains have large carnivore damage. Hyenas left bones in repeating similar tooth mark and crush damage stages, demonstrating a butchering/bone cracking strategy. The femora of subadult cave bears are intermediate in damage patterns, compared to the adult ones, which were fully crushed to pieces. Hyenas produced round–oval puncture marks in cub femora only by the bone-crushing premolar teeth of both upper and lower jaw. The punctures/tooth impact marks are often present on both sides of the shaft of cave bear cub femora and are simply a result of non-breakage of the slightly calcified shaft compacta. All stages of femur puncturing to crushing are demonstrated herein, especially on a large cave bear population from a German cave bear den.

2. Introduction

2.1 First ‘bone flute descriptions’

The first ‘Neanderthal cave bear bone flute’ from the Middle Palaeolithic was believed to have been discovered in the 1920s from Potočka Zijalka Jama Cave (i.e. Potok Cave), Slovenia [1]. This was a larger cave bear den (cf. [2,3]) and Late Palaeolithic Aurignacian (not Neanderthal) used rock shelter camp site at the entrance (cf. [1]; figure 1). In this cave, cave bear hunts by Cro-Magnon humans seem to be indicated on a cave bear shoulder blade pathology (large diagonal impact hole, partly healed diagonal hole) that seems to have been made by a probable Mladeč projectile bone point [5].

Figure 1.

Figure 1. Studied and referred Late Pleistocene (MIS3–5d) European cave sites with ‘Palaeolithic cave bear pseudo-bone flutes’, and compared cave bear dens with hyena influence (hyena palaeobiogeography of 150 sites [4]).

Other cave bear cub femora with holes (‘bone flutes’) were then reported from the Istállóskö Cave, Hungaria (cf. [6]). This was a smaller cave bear and Ice Age spotted hyena (Crocuta crocuta spelaea) carnivore den which overlaps with another Aurignacian camp site, but again, it has no Middle Palaeolithic Neanderthal occupation signs (cf. [7]).

Brodar [8] reported cave bear cub femora and other cave bear bones ‘with holes’ as further proof of the ‘oldest instruments in the world’ from the Mokriška Jama Cave (or Medvedja Jama Cave=Bear Cave), Slovenia. Also, this is a large cave bear den which had again an Aurignacian camp site at the entrance, and again no Neanderthal occupation at all (cf. [9,10]).

All aforementioned femora and other cave bear bones with ‘holes’ (i.e. ribs, humeri and jaws) were compiled and studied by the ethnologist/musician Omerzel-Telep [11], without any natural science, nor palaeozoology background, especially the important ecology of cave bears and their predators/scavengers, non-human top predators of the Ice Age and the wide distribution of cave bear den caves in Europe (cf. [3,1221]; figures 1 and 2), where always large amounts of damaged and also punctured cave bear bones are present, such as figured with many new examples herein for the northern German Weiße Kuhle Cave and other cave bear dens (figures 37).

Figure 2.

Figure 2. Cave bear scavenging models in larger cave bear den caves (here Zoolithen Cave, Germany) for all three top predators that hunted, killed and scavenged on cave bears all over Europe within caves in boreal forest palaeoenvironments. The bone crusher of longbones was only the Ice Age spotted hyena, which produced round/oval puncture marks on cave bear cub bones by the bone crushing premolar teeth, i.e. ‘bone flute holes’ (composed and adapted from [4,14,15,22,23]; illustrations G. Teichmann).

Figure 3.

Figure 3. Carnivore puncture holes in cave bear skulls, jaws and postcranial bones caused by top predator canine teeth (lions, leopards, hyenas and wolves), but are mainly products at longbones and lower jaws of the premolar cracking teeth of hyenas (cf. figure 2). (1) Cub skull (small cave bear form U. spelaeus eremus) from the Weiße Kuhle Cave, Germany, which was scavenged strongly on the left side. Puncture holes are produced by canines (in cranium), whereas the breakage of the left mandible is the result of hyena premolar cracking teeth. (a) Dorsal, (b) lateral, (c) detail of lateral tooth mark holes (produced by carnivore canines, best fitting to hyenas or lions) (PAL collection). (2) Single probably canine impact of a large carnivore (lion, hyena) on a cub skull (large cave bear form U. ingressus) from the Große Teufels Cave, Germany. (a) Dorsal, (b) lateral, (c) detail of tooth mark hole (GTCP collection). (3) Mandible (U. s. eremus) from the Weiße Kuhle Cave of a cub with hyena premolar impact holes (cracking purpose). Such mandibles were crushed always similar with damaging the ramus, or flakes of the lower distal mandible. (a) Lateral outer view, (b) lateral inner view, (c–e) details of puncture holes of both sides and (f) refitting of the jaw with all tooth marks of both sides projected in one level which fit in one tooth mark of the bone crushing teeth of the upper jaw of a hyena (all PAL collection).

2.2 The long discussed Slovenian punctured cave bear cub bone find

Another juvenile bear cub femur with holes from Divje Babe I Cave, Slovenia, a small cave bear den (cf. [25]; figure 5(4)), where also Neanderthal Mousterian layers were believed to be present [26], was declared twice incorrectly as the ‘oldest instrument’, a 43 140 BP old ‘Neanderthal flute’ from layer 8 [26,27] (figure 5(4)). This was already contradictory to the results of the archaeological inventory that is well acceptably declared to be solely of, again, Cro-Magnon human Late Palaeolithic origin, and not of Mousterian (cf. [28]). The Aurignacian lithic material appears also together with cave bear remains [25]. Therefore, there is no evidence for a Neanderthal (Mousterian) context and the cave bear remains, which even occur in several older and younger Late Pleistocene layers (cf. [25]). The only absolute date was made solely on a cave bear bone, the ‘bone flute’, whose age would date into the Neanderthal or ‘cave bear den’ time period. This report of a ‘cave bear femur bone flute’ was not the ‘oldest’, neither historically, nor by stratigraphy. The bone's holes on the dorsal side appear not to line up, whereas on the ventral side another hole was declared as the ‘thumb hole’. The studies even thrilled up to ‘exact musical studies’ [29]. Fink [30,31] declared then to the top of this, without natural scientific studies, that the hole spacing matched a ‘diatonic scale sequence, among the most widespread scales known’—which underlines, also contradictory, that this is not of human origin. Ethnologist/musicians created then a wave of ‘cave bear bone instruments’ based solely on ‘holes in bones’ (compiled in [11]), from all kinds of carnivore punctured cave bear bones, even other than femora. Other authors doubted the ‘flute’ and human origin however (e.g. [3238]) or were fighting for pro-arguments (e.g. [39,40]). At least, very correctly, the ‘holes’ were mostly discussed to be of ‘carnivore chewing damage’ origin (cf. [32,33,37,41]), whereas X-ray scans did not prove any ‘drill-scratches around the holes’ or any marks of stone tools on the bones, and left again the question of the hole origin open (cf. [42]). The exact carnivore was never estimated, even by newer and fully controversial studies by Turk et al. [24] that lack carnivore ecology knowledge, especially in tooth and jaw function of top predators. Ignoring the top predator bone damage on Ice Age animal bones, again the pseudo-bone flute was not only ‘confirmed’, even more bone flute finds were added by the same Slovenian author (cf. [43]), who misidentified: (a) the site occupation by Neanderthals, as those of Aurignacians [28], (b) the bone, by rotating it upside down (see [44]), the 180° rotation of which is corrected herein (figure 5a), (c) the general bone taphonomy of cave bear bones, and (d) carnivore jaw functions, especially hyenas, correctly presented herein (figure 2).

2.3 Hyena and cave bear populations over Europe: specialized cave bear scavenges

In this contribution, not only sole carnivore damage can be demonstrated on all previously published ‘pseudo-bone flutes’, which were already revised in some cases [4,16] (figure 2). Herein, even more of such cave bear bones with holes can be added with focus only on the femora (figures 57), from German and Romanian cave bear den sites (therefore not limited to Slovenia at all, as mentioned by Turk et al. [24]; see figures 1, 57 and table 1). Their producer, a large carnivore, and the main scavenger/bone destructor of the Ice Age, the Ice Age spotted hyena Crocuta crocuta spelaea, will be discussed as the oval hole producer herein (figure 2), based on the intensive Late Pleistocene central European cave bear and top predator studies in and outside caves of the past years (e.g. [3,121622,51,54,55]). This results in a different viewpoint of modern zooarchaeology, multiple animal/human use of larger cave systems and cave models (figure 2). The Ice Age top predator research in Europe focused these past years on hunting of cave bears in large cave bear dens. There, damage on cave bear bones is now well known and reported in several publications (e.g. [3,4,16,1821,51,56]; figure 2). All former archaeological, ecological focus cave bear ‘bone flute’ studies forgot all four cave bear predators—steppe lions (Panthera leo spelaea), leopards (Panthera pardus spelaea), Ice Age spotted hyenas (Crocuta crocuta spelaea) and Ice Age wolves (Canis lupus spelaeus)—which are known now to be cave bear killers, and main consumers in mountain regions, where mammoth steppe megafauna were absent [4,1821]. These predators specialized in consuming mainly (and especially in winter times during cave bear hibernation) cave bears in boreal forest mountain regions, but in different ways and with different impact on the carcasses and bone destruction (cf. figures 2 and 3). However, the main ‘bone destructor’ is known to be the European Ice Age spotted hyena [19] (figure 2), with cave bear bone damage first understood at the overlapping hyena den (cave entrance) and cave bear den of the Perick Caves [5052], with newer proof at Sophie's Cave [21,22], and Hermann's Cave [16] or Zoolithen Cave [18] and herein best demonstrated and newly added for the Weiße Kuhle Cave (figures 3, 4, 6 and 7).

Table 1.

Studied and from literature compiled cave bear, hyena, wolf den sites with pseudo-bone flutes (i.e. punctured cave bear cub femora), and overlap of Late Palaeolithic Aurignacian camp sites at the cave entrances, or cave bear hunt signs deep in caves. ‘Pseudo-bone flutes’ are not in Middle Palaeolithic archaeological, but of Late Palaeolithic and cave bear den context with large carnivore influence.

Figure 4.

Figure 4. Carnivore puncture holes in cave bear (U. s. subsp. and U. ingressus) longbones (humerus, radius, tibia) and pelvic and pedal bones by top predator (lions, leopards, hyenas and wolves) canine and mainly premolar hyena teeth. (1–4) Cub humeri from the Weiße Kuhle Cave, Germany. (5–6) Cub radi from the Weiße Kuhle Cave, Germany. (7–11) Cub tibiae from the Weiße Kuhle Cave, Germany. (12) Cub coxa from the Weiße Kuhle Cave, Germany. (13–14) Cub and adult calcanei from the Weiße Kuhle Cave, Germany (all PAL collection).

Figure 5.

Figure 5. Pseudo ‘Neanderthal bone flutes’ of different aged cave bear (U. s. subsp. and U. ingressus) cub femora (less than 1 year individual age) from various European large cave bear den sites. (1) Femur from Mokriška Jama Cave, Slovenia (photos adapted from [24]; NMLS collection). (2) Femur from Keppler Cave, Germany (photos adapted from [4]; SMM collection). (3) Femur from Sophie's Cave, Germany (photos adapted from [22]; SMM collection). (4) Femur from Divje Babe Cave 1—‘the Neanderthal bone flute holotype’, Slovenia (photos from NMLS collection). (5) Femur from Oase Cave, Romania (IR collection). (6) Femur from Hermann's Cave, Germany (photos adapted from [16]; RC collection).

Figure 6.

Figure 6. Continuous documentation of destruction stages of cave bear (U.s. subsp. and U. ingressus) cub femora: (1–7) puncture, (8–9) part-flake, (10–14) full breakage-flakes—all with puncture holes or half preserved holes after splitting in flakes—of different aged cave bear cub femora (less than 1 year individual age) and different species (U. s. eremus and U. ingressus)—all from the Weiße Kuhle Cave, Germany (PAL collection).

Figure 7.

Figure 7. Examples of the destruction stages of femora of cave bear cubs, subadult to adult cave bears (U. s. subsp. and U. ingressus). (1) This femur of an adult cave bear (U. s. eremus) from the Große Teufels Cave, Germany (PO collection), is the best proof for the hyena tooth mark and damage origin, where two diagonal tooth marks (i.e. diagonal cut) can be reconstructed, and where lower and upper jaw premolar teeth and their antagonistic tooth mark impact holes fit exactly to the hyena skull dentition. A hyena tried to cut the distal joint. (a) Cranial view, (b) detail of the cranial tooth mark holes, (c) caudal view, (d) detail of the caudal tooth mark holes, (e) reconstruction refitting of the P-teeth into the cranial and caudal tooth pits, demonstrating exact fitting and two overlapping diagonal tooth marks (GTCP collection). (2) Proximally chewed and punctured femur joint of a subadult cave bear (U. s. spelaeus or U. ingressus) from the Weiße Kuhle Cave, Germany. The impact marks are two types: (a) full and deep into the spongiosa, i.e. tooth with intact crown tip); (b) round surface breakages of compacta, i.e. tooth with rubbed or damaged tip or slight impact (PAL collection). (3) Cut of proximal joint (U. s. eremus) demonstrated at a femur from the Keppler Cave, Germany, cranial (SMM collection). (4) Shaft from the Oase Cave, Romania, cranial (IR collection). (5) Shaft of a subadult (large cave bear U. ingressus) with distally cracked parts (all found in the cave close to each other with old fractures) from the Weiße Kuhle Cave, Germany, cranial (PAL collection). (6) Selected femur fragments of cub to subadult cave bears (U. s. eremus and U. s. subsp.) partly with spiral breakage, and tooth mark impact marks on the surfaces from the Weiße Kuhle Cave, Germany (PAL collection). (7) Many selected femur fragments of subadult to adult cave bears (U. s. eremus and U. s. subsp.) partly with spiral breakage, and tooth mark impact marks on the surfaces from the Perick Caves, Germany (PCH collection).