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螺旋咬合平面的自然史及其在早期人类中的演变。

The natural history of the helicoidal occlusal plane and its evolution in early Homo.

作者信息

Tobias P V

出版信息

Am J Phys Anthropol. 1980 Aug;53(2):173-87. doi: 10.1002/ajpa.1330530202.

DOI:10.1002/ajpa.1330530202
PMID:6774617
Abstract

In modern man the pitch of the occlusal plane may vary along the tooth-row. When anterior cheek-teeth show a plane sloping upward palatally, whilst that on posterior cheek-teeth slopes upward buccally, there results a twisted or helicoidal occlusal plane (Ackermann). Several hypotheses have been proposed for the structural basis of the helicoidal occlusal plane. Campbell's proposal ('25) has gained widest acceptance, namely that the helicoid results from anteroposterior differences in upper and lower alveolar arch width. In the early 1960s, while studying the Olduvai hominids assigned to Homo habilis, the author noted changing occlusal slopes along the tooth-row and a slight helicoid, although these featues had not been noted in other early hominids. Subsequently, Wallace showed a total absence of the helicoid from South African australopithecines, and its presence in Swartkrans Homo, SK 45 and SK 80. Recent studies confirm the presence of the helicoid in all available specimens of H. habilis, including Stw 53 found at Sterkfontein in 1976. Hence, this trait may distinguish between Australopithecus and early Homo. Measurements of the maxillary arch widths have shown that, whereas in Australopithecus arch widths increase to a maximum at M3, in early Homo maxillary arch widths are greatest at M2. The decline in posterior maxillary arch width is part of a general reduction of that region. Thus despite striking elongation of premolars and M1 in early Homo, M2 and M3 are mesiodistally abbreviated. It is hypothesized that the onset of posterior arch reduction, with the appearance of a helicoid, was a structural and functional concomitant of the transition from the presumed australopithecine ancestor to H. habilis.

摘要

在现代人中,咬合平面的倾斜度可能会沿着齿列发生变化。当前臼齿的平面腭侧向上倾斜,而后臼齿的平面颊侧向上倾斜时,就会形成扭曲或螺旋状的咬合平面(阿克曼)。关于螺旋状咬合平面的结构基础,已经提出了几种假说。坎贝尔的提议(1925年)得到了最广泛的认可,即螺旋状是由上下牙槽弓宽度的前后差异导致的。20世纪60年代初,在研究被归类为能人属的奥杜威古人类时,作者注意到沿着齿列咬合倾斜度的变化以及轻微的螺旋状,尽管在其他早期古人类中并未注意到这些特征。随后,华莱士发现南非南方古猿完全没有螺旋状,而在斯瓦特克朗斯的能人属(SK 45和SK 80)中存在螺旋状。最近的研究证实,在所有现有的能人属标本中都存在螺旋状,包括1976年在斯特克方丹发现的Stw 53。因此,这一特征可能区分南方古猿和早期人类。对上颌弓宽度的测量表明,在南方古猿中,上颌弓宽度在M3处增加到最大值,而在早期人类中,上颌弓宽度在M2处最大。上颌后弓宽度的减小是该区域普遍缩小的一部分。因此,尽管早期人类的前磨牙和M1显著伸长,但M2和M3在近远中方向上缩短。据推测,后弓缩小的开始以及螺旋状的出现,是从假定的南方古猿祖先向能人属过渡的结构和功能伴随现象。

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