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50<br />

Si 5<br />

15i<br />

10-<br />

5-<br />

20<br />

J 15<br />

I 10<br />

f 5<br />

Humeri Femora<br />

•i.llllll.<br />

73 75 77 79 81 83 85<br />

Length mm<br />

Ulnae<br />

I.I.I<br />

73 75 77 79 81 83 85<br />

Length mm<br />

Carpometacarpi<br />

•••••••I.I I" i" i~ i — i — i — i r*~i—•—i<br />

36 37 38 39 40 41 42<br />

Length mm<br />

a 4<br />

I<br />

SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY<br />

15-<br />

JUV<br />

10-<br />

26.5 27.5 28.5 29.5 30.5 31.5<br />

Length mm<br />

Tibiotarsi<br />

• -III.<br />

• i<br />

48 50 52 54 56<br />

15-,<br />

g 10<br />

o<br />

3<br />

| 5<br />

u.<br />

0<br />

Length mm<br />

Tarsometatarsi<br />

• -Mil..<br />

31 32 33 34 35 36<br />

Length mm<br />

FIGURE 8.—Histograms of lengths of Pterodroma mollis bones from Amsterdam Island<br />

more robust than in the similar-sized P. neglecta. Pterodroma<br />

baraui differs from P. arminjoniana in that the ventral process<br />

of the os lacrimale, where it descends from the os ectethmoidale,<br />

is much shorter, with a different shape of the articular facet.<br />

The lower fonticulus orbitocranale is more elongate in P<br />

baraui {n=3, 5.8 mm high x 9.1 mm long, 6.0 x 8.6 mm, 6.0 x<br />

8.8 mm, vs. 6.5 x 7.7 mm in P. arminjoniana). The fossil cranium<br />

from site 8.11 has a basicranial length of 37 mm but is too<br />

broken to measure further; however, the extensive temporal<br />

fossae, lacrimal shape, and shape of the fonticulus orbitocraniale<br />

clearly identify it as P baraui. The posterior portion of the<br />

cranium from site 8.3 (width at zygomatic processes 25.5 mm)<br />

has wide temporal fossae like P. baraui and is referred to that<br />

species. The postcranial bones in P. baraui and P. arminjoniana<br />

are very similar, and subtle differences, if present, between<br />

them would not be of use in identifying fossil material that is<br />

worn, weathered, or broken. Because all cranial material from<br />

site 8 is referred to P. baraui, all the postcranial bones of midsized<br />

Pterodroma from this site also are referred to that species<br />

(Table 3). This is further supported by the tarsometatarsi from<br />

site 8, which are similar to those of P. baraui (Table 4) and are<br />

shorter and stouter than those of P. macroptera.<br />

TABLE 3.—Summary statistics for bones attributed to fossil Pterodroma baraui<br />

and measurements (mm) of intermediate-sized fossil Pterodroma species,<br />

Amsterdam Island.<br />

Species<br />

P. baraui<br />

mean<br />

standard deviation<br />

minimum<br />

maximum<br />

sample size<br />

P. arminjoniana/<br />

baraui<br />

site 18.1<br />

site 18.27<br />

site 18.26<br />

P. arminjoniana<br />

site 18.2<br />

site 18.8<br />

site 18.11<br />

Fern L<br />

32.87<br />

0.05<br />

32.83<br />

32.9<br />

2<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

TmtL<br />

38.14<br />

0.06<br />

38.1<br />

38.18<br />

2<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

HumL<br />

91.82<br />

1.82<br />

90.4<br />

94.32<br />

4<br />

-<br />

95.4<br />

95.8<br />

-<br />

89.7<br />

91.5<br />

Pterodroma sp.<br />

UlnaL<br />

97.42<br />

1.99<br />

95<br />

102.5<br />

13<br />

96.8<br />

- -<br />

97.3<br />

-<br />

-<br />

Cmc L<br />

47.62<br />

1.36<br />

46<br />

50.1<br />

9<br />

-<br />

- -<br />

- -<br />

-<br />

CorL<br />

26.07<br />

0.42<br />

25.6<br />

26.43<br />

3<br />

Two premaxillae (MNZ S34852, MNZ S34859) are very<br />

short and stout and are not referable to any of the above species.<br />

Bourne (1968) gave measurements for a premaxilla of the<br />

- --<br />

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