Agrippina wrote:The reason I heard them give for it's not being 'homo' but rather Australopithecine is because of the arms, they're longer than they would be for 'homo.' Or rather that was one reply I heard them give there were others, but I don't remember so I won't commit myself but I do remember about the arms.
Well, here's what the paper itself has to say on this point.
Lee R. Berger, Darryl J. de Ruiter, Steven E. Churchill, Peter Schmid, Kristian J. Carlson, Paul H. G. M. Dirks, Job M. Kibii, Australopithecus sediba: A New Species of Homo-Like Australopith from South Africa, Science 9 April 2010:
Vol. 328. no. 5975, pp. 195 - 204, DOI: 10.1126/science.1184944.
Although the skull and skeleton of Au. sediba do evince derived features shared with early Homo, the overall body plan is that of a hominin at an australopith adaptive grade. This supports the argument, based on endocranial volume and craniodental morphology, that this species is most parsimoniously attributed to the genus Australopithecus.
So the major reasons for retaining sediba within Australopithecus, according to the authors, were:
1. The overall body plan remains that of a hominin at an australopith adaptive grade.
2. Endocranial volume (brain size) remained small.
3. Craniodental morphology (skull and teeth forms, as can best be seen in the photographs comparing the full-face views of the sediba skulls with those of Au. africanus and other early skulls., to which I linked earlier).
With regard to point 1, the authors say:
Postcranially, Au. sediba is similar to other australopiths in its small body size, its relatively long upper limbs with large joint surfaces, and the retention of apparently primitive characteristics in the upper and lower limbs
With regard to point 2:
The minimum cranial capacity of MH1 is estimated at 420 cm3.
On a comparative scale, the authors characterized the cranial capacity of each of the recognized Au. species -- including sediba -- as "small," of H. habilis as "intermediate, and of H. rudolfensis and H. erectus as "large." In their supplementary material (Supplementary Text S4), the authors note that:
Taxonomic diagnoses and phylogenetic interpretations are generally
based on craniodental remains, which necessitate such a focus even in taxa such as Au. sediba
that preserve a more complete representation of the skeleton. This is not to say, however, that
postcranial attributes cannot enlighten phylogenetic studies, and for these reasons the
significance of the postcranial morphology of Malapa is discussed. What is important is that the
postcranial remains support phylogenetic inferences derived from study of the craniodental
material.
Note, with regard to point 3, that the authors say:
The closest morphological comparison for Au. sediba is Au. africanus, as these taxa share numerous similarities in the cranial vault, facial skeleton, mandible, and teeth.
Also, wrt point 3, the authors note that:
...we consider Au. sediba to be more appropriately positioned within Australopithecus, based on the following craniodental features: small cranial capacity, pronounced glabelar region, patent premaxillary suture, moderate canine jugum with canine fossa, small anterior nasal spine, steeply inclined zygomaticoalveolar crest, high masseter origin, moderate development of the mesial marginal ridge of the maxillary central incisor, and relatively closely spaced premolar and molar cusps.
This is not a long article, though it is, of course, full of technical anatomical terms (some of these, at least, will be familiar to most RatSkeppers, others become obvious in context or from study of the photos and figures). It should be perfectly possible for anyone with an interest and some modest background in the area to follow the article's gist. The article is open access (you have to register with the AAAS, the American Assoc. for the Advancement of Science, but registration is free):
http://www.sciencemag.org/cgi/content/full/328/5975/195#T1 The supplementary discussions are also accessible online: http://www.sciencemag.org/cgi/content/full/328/5975/195/DC1
I would recommend the article as the starting point for informed discussion, rather than interviews, blog posts, forum discussions, and other second-hand sources. As valuable as some of the latter are -- particularly the views of other anthropologists and paleontologists such as John Hawks or laelaps -- they are all based ultimately on the published articles (there is another one about the geological and ecological context, and dating of the strata, in which the fossils were found) and the supplementary materials that accompany them.
The authors performed a careful comparison of the craniodental characters of Au. sediba with the following fossils (Supp. Text S2):
Au. afarensis. The samples attributed to Au. afarensis from Hadar, Laetoli, and the Middle
Awash were utilized. For this taxon we relied on published reports (7) and casts.
Au. africanus. The samples attributed to Au. africanus from Taung, Sterkfontein and
Makapansgat were employed. Original specimens were examined first-hand.
Au. garhi. The cranium BOU-VP-12/130 from Bouri was included, with data taken from a
published report (8).
Au. aethiopicus. The cranium KNM-WT 17000 was examined first-hand for this study.
Au. boisei. Samples from the Omo Shungura sequence, East Lake Turkana, and Olduvai Gorge
were included in this study. Original specimens from East Lake Turkana were examined firsthand,
while casts and published reports (9) were used to study the Omo and Olduvai materials.
Au. robustus. The samples from Kromdraai, Swartkrans, Sterkfontein, Drimolen, Gondolin, and
Coopers were included in this study. First-hand observations of original specimens from all
localities were used with the exception of Drimolen fossils, which were compared using
published reports (10, 11).
H. habilis. Samples from Olduvai Gorge, East Lake Turkana, the Omo Shungura sequence, and
Hadar were included in this study. Original East Lake Turkana fossils were examined first-hand,
while for the Olduvai, Omo, and Hadar materials we relied on casts and published reports (12,
13, 14). We include the following fossils in the hypodigm of H. habilis: AL 666-1, KNM-ER
1478, KNM-ER 1501, KNM-ER 1502, KNM-ER 1805, KNM-ER 1813, KNM-ER 3735, OH 4,
OH 6, OH 7, OH 13, OH 15, OH 16, OH 21, OH 24, OH 27, OH 31, OH 37, OH 39, OH 42,
OH 44, OH 45, OH 62, and OMO-L894-1.
H. rudolfensis. Samples from Olduvai Gorge, East Lake Turkana, and Lake Malawi were
included in this study. The East Lake Turkana fossils were examined first-hand, while for the
Olduvai and Lake Malawi fossils we relied on casts and published reports (15, 16). We include
the following fossils in the hypodigm of H. rudolfensis: KNM-ER 819, KNM-ER 1470, KNMER
1482, KNM-ER 1483, KNM-ER 1590, KNM-ER 1801, KNM-ER 1802, KNM-ER 3732,
KNM-ER 3891, OH 65, and UR 501.
H. erectus. Samples from Baringo, Chemeron, Dmanisi, East and West Lake Turkana, Konso,
Olduvai Gorge, Sangiran, Swartkrans, Tighenif, Trinil, and Zhoukoudian were included in this
study. In particular, the following specimens from Swartkrans are considered to represent Homo
erectus: SK 15, SK 18a, SK 27, SK 43, SK 45, SK 68, SK 847, SK 878, SK 2635, SKW 3114,
SKX 257/258, SKX 267/2671, SKX 268, SKX 269, SKX 334, SKX 339, SKX 610, SKX 1756,
SKX 2354, SKX 2355, SKX 2356, and SKX 21204. It has been suggested (17, 18) that SK 847
and Stw 53 might represent the same taxon, and that this taxon is a currently undiagnosed
species of Homo in South Africa. However, we agree with Clarke (19, 20) that SK 847 can be
attributed to H. erectus, and that Stw 53 represents A. africanus. Since there is no clear indication
that more than one species of Homo is represented in the Swartkrans sample, we consider all this
material to belong to H. erectus. Original Baringo, Chemeron, Lake Turkana and Swartkrans
fossils were all examined first-hand, while the remainder were based on casts and published
reports (21, 22, 23, 24, 25).
Not only is this list revealing of the care taken by the authors to examine and compare all the relevant fossil material, please also note the sheer wealth of fossil material for this timeframe (not including any of the Ardi material or even earlier fossils, or erectus or other fossils from Eurasia, or archaic human (antecessor, heidelbergensis, rhodesiensis) fossils from any place or time, or neanderthal fossils, or early anatomically modern human fossils of the last couple of hundred thousand years for any place or time), for the next time you hear from some YEC apologist that the fossil support for the evolutionary picture of human ancestry could all fit in a "drawer" or a "shoebox."