图:Bruno Souza pesquisador · CC BY-SA 4.0 · Wikimedia Commons
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羚羊河南方古猿种
Australopithecus bahrelghazali
羚羊河南方古猿,又名南方古猿羚羊河种、加扎勒河南方古猿或南方古猿加扎勒河种是人科的化石,最初于1993年由古生物学家米歇尔·布吕内在乍得的加扎勒河发现。这次发现了一个下颌骨碎片、第二下门齿、两颗下犬齿及所有四颗的前臼齿,这些牙齿都仍在腭龈内。这个标本编号为KT-12/H1,布吕内为了纪念他的同窗而将这个标本命名为“Abel”。发现这个标本的位点是在东非大裂谷以西约2500公里,估计属于300-350万年前。
摘自维基百科「羚羊河南方古猿」,CC BY-SA 4.0
- 学名
- Australopithecus bahrelghazali
- 分类等级
- 种
- 上级类群
- 南方古猿属
- 大类
- 哺乳动物
- 数据库
- GBIF
百科正文
羚羊河南方古猿的下颌骨很像阿法南方古猿,故有指它根本不是一个新的物种,而只是属于阿法南方古猿的变种范围内。1996年,布吕内将KT 12/H1定为羚羊河南方古猿的原模标本。但是,由于布吕内将这个标本关起来,以致与1999年的国际动物命名法规有所抵触,故此他的说法难以证明。羚羊河南方古猿是唯一在中非发现的南方古猿类,故此早期人类演化可能有第三个起源点。
以上内容摘自维基百科「羚羊河南方古猿」,按 CC BY-SA 4.0 使用,去掉了参考文献、外部链接等尾部小节,公式改写成了纯文本。全文、配图和出处见原文。
英文维基百科补充中文条目比较短,下面是英文条目「Australopithecus bahrelghazali」的原文
Australopithecus bahrelghazali is an extinct species of australopithecine discovered in 1995 at Koro Toro, Bahr el Gazel, Chad, existing around 3.5 million years ago in the Pliocene. It is the first and only australopithecine known from Central Africa, and demonstrates that this group was widely distributed across Africa as opposed to being restricted to East and southern Africa as previously thought. The validity of A. bahrelghazali has not been widely accepted, in favour of classifying the specimens as A. afarensis, a better known Pliocene australopithecine from East Africa, because of the anatomical similarity and the fact that A. bahrelghazali is known only from 3 partial jawbones and an isolated premolar. The specimens inhabited a lakeside grassland environment with sparse tree cover, possibly similar to the modern Okavango Delta, and similarly predominantly ate C4 savanna foods—such as grasses, sedges, storage organs, or rhizomes—and to a lesser degree also C3 forest foods—such as fruits, flowers, pods, or insects. However, the teeth seem ill-equipped to process C4 plants, so its true diet is unclear.
Research history
In 1995, two specimens were recovered from Koro Toro, Bahr el Gazel, Chad: KT12/H1 or "Abel" (a jawbone preserving the premolars, canines, and the right second incisor) and KT12/H2 (an isolated first upper premolar). They were discovered by the Franco-Chadian Paleoanthropological Mission, and reported by French palaeontologist Michel Brunet, French geographer Alain Beauvilain, French anthropologist Yves Coppens, French palaeontologist Emile Heintz, Chadian geochemist engineer Aladji Hamit Elimi Ali Moutaye, and British palaeoanthropologist David Pilbeam. Based on the wildlife assemblage, the remains were roughly dated to the middle to late Pliocene 3.5–3 million years ago; consequently, the describers decided to preliminarily assign the remains to Australopithecus afarensis, which inhabited Ethiopia during that time period, barring more detailed anatomical comparisons. In 1996, they allocated it to a new species, A. bahrelghazali, naming it after the region; Bahr el Gazel means "River of the Gazelles" in classical Arabic. They denoted KT12/H1 as the holotype and KT12/H2 a paratype.
Anatomy
The teeth of KT12/H1 are quite similar to the jawbone of A. afarensis, with large and incisor-like canines and bicuspid premolars (as opposed to molar-like premolars). Unlike A. afarensis, the alveolar part of the jawbone where the tooth sockets are is almost vertical as opposed to oblique, possesses poorly developed superior transverse torus and moderate inferior torus (two ridges on the midline of the jaw on the tongue side), and thin enamel on the chewing surface of the premolars. Brunet and colleagues had listed the presence of 3 distinct tooth roots as a distinguishing characteristic, but the third premolar of the A. afarensis LH-24 specimen from Middle Awash, Ethiopia, was described in 2000 as having the same feature, which shows that premolar anatomy was highly variable for A. afarensis. The mandibular symphysis (at the midline of the jaw) of KT40, especially, as well as KT12/H1 have the same dimensions as the symphysis of A. afarensis, though theirs is relatively thick compared to the height.
Palaeoecology
Carbon isotope analysis has shown that A. bahrelghazali had high δ13C values. This indicates a diet of predominantly C4 savanna foods, such as grasses, sedges, underground storage organs (USOs), or rhizomes. There is a smaller C3 portion which may have comprised more typical ape food items such as fruits, flowers, pods, or insects. This indicates that, like contemporary and future australopiths, A. bahrelghazali was capable of exploiting whatever food was abundant in its environment, whereas most primates (including savanna chimps) avoid C4 foods. However, despite 55–80% of δ13C deriving from C4 sources similar to Paranthropus boisei and the modern gelada (and considerably more than any tested A. afarensis population), A. bahrelghazali lacks the specialisations for such a diet. Because the teeth are not hypsodont, it could not have chewed large quantities of grass, and because the enamel is so thin, the teeth would not have been able to withstand the abrasive dirt particles of USOs.
以上节选摘自英文维基百科「Australopithecus bahrelghazali」,按 CC BY-SA 4.0 使用,去掉了参考文献、外部链接等尾部小节,公式改写成了纯文本。篇幅所限,较长的小节只摘了开头一部分,有的小节没有收;全文、配图和出处见原文。