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NUMBER 89 191<br />
FIGURE 4.—Holotypical right carpometacarpus (UF 30015) of Aquila bivia<br />
from Inglis IA, Citrus County, Florida, in internal (left) and external (right)<br />
views. Scale=xl, bar=l cm.<br />
UF 30031-30033; two proximal ends of right femora, UF<br />
30020, 30021; distal end of right femur, UF 30022; left femur,<br />
UF 30019 (Figure 5B; Table 2); right tibiotarsus, UF 30012<br />
(Figure 5A; Table 2); proximal end of right fibula, UF 30013;<br />
right metatarsal I, UF 30018; right phalanx 1 of digit I, UF<br />
30016; left ungual phalanx of digit II, UF 30017; right phalanx<br />
2 of digit II, UF 30045; left phalanx 1 of digit III, UF 30046;<br />
phalanx 3 of digit III, UF 30044; phalanx 1 of digit IV, UF<br />
30047; ungual phalanx of digit IV, UF 30048. At least two<br />
adults represented.<br />
Ill Ranch (East Ravine at Dry Mountain, Graham County,<br />
Arizona (OMNH <strong>Lo</strong>cality V818; Figure 2)): Partial associated<br />
skeleton (OMNH 50271) including proximal and distal ends<br />
of a right carpometacarpus, right and left ulnares, right radiale,<br />
proximal end of left tarsometatarsus; right metatarsal I, phalanx<br />
1 and ungual of digit I, phalanx 2 and ungual of digit II, phalanges<br />
1-3 and ungual of digit III, phalanges 2-4 and ungual of<br />
digit IV; left metatarsal I and phalanx 1 of digit I, phalanx 2<br />
and ungual of digit II, phalanx 3 (partial) of digit III, and phalanges<br />
2-4 of digit IV.<br />
This locality is within greenish clay in the Gila Conglomerate<br />
at the approximate level of paleomagnetic samples 112 and<br />
113, East Ravine, of Galusha et al. (1984). This section has reversed<br />
polarity throughout and represents Chron C2r, or slightly<br />
above the 2.47 Ma Dry Mountain Ash Bed (Izett, 1981; Galusha<br />
et al., 1984; Tomida, 1987). One adult (from associated<br />
material) is represented.<br />
MEASUREMENTS OF PARATYPES.—See Table 1.<br />
ETYMOLOGY.—From Latin, bivius, -a, -um, two-wayed, in<br />
reference to the distribution of the fossil specimens in Florida<br />
and Arizona.<br />
DIAGNOSIS.—The species is diagnosed by the following<br />
characters. Carpometacarpus (UF 30015, OMNH 50271; Figure<br />
4) with relatively deep external ligamental attachment with<br />
pronounced proximal border, metacarpal I relatively long and<br />
robust, pit below pollical facet on metacarpal II, relatively<br />
large prominence for muscle attachment of proximal internal<br />
edge of metacarpal III (ligamental attachment shallow and<br />
proximal border less pronounced, metacarpal I relatively shorter<br />
and less robust, absence of pit below pollical facet on metacarpal<br />
II, and prominence for muscle attachment small in Aquila<br />
chrysaetos, A. rapax, A. heliaca, A. verreauxii, and A. audax).<br />
Femur with relatively long and slender shaft (shaft shorter and<br />
more robust in A. chrysaetos) and with broad, deeply excavated<br />
popliteal area (area narrower and moderately excavated in A.<br />
chrysaetos; Figure 5B). Tibiotarsus with relatively long, narrow<br />
shaft (shaft shorter and more robust in A. chrysaetos; Figure<br />
5A). Size relatively large compared with Aquila chrysaetos,<br />
A. rapax, A. heliaca, A. verreauxii, or A. audax.<br />
COMPARATIVE MATERIAL.—Haliaeetus leucocephalus (Linnaeus);<br />
USNM 611999, USNM 489276, 1 male and 1 female.<br />
Aquila rapax (Temminck), USNM 430406, 430532, 488147,<br />
488148, 1 male, 3 females. Aquila heliaca Savigny, USNM<br />
488808, female. Aquila chrysaetos (Linnaeus), UF 19399,<br />
23961,23962,23964,1 male, 3 females; USNM 17721,17983,<br />
18194, 18802, 19251, 19394, 19399, 19724, 19777,288513,<br />
319967, 320978, 343130, 491476, 500354, 500355, 500367,<br />
502292,612086, 5 males, 5 females, 9 unsexed; LACM 89953,<br />
female. Aquila audax (Latham), USNM 344883, unsexed. Aquila<br />
verreauxii Lesson, USNM 612539, unsexed.<br />
STATUS.—Extinct, known from fossils only.<br />
REMARKS.—Aquila bivia was a large eagle that was closely<br />
related to the Golden Eagle {A. chrysaetos), but it was<br />
10%-15% larger than females of that species and had limb elements<br />
that do not overlap with those of A. chrysaetos in length<br />
(Table 2). A large series of late Pleistocene eagle bones from<br />
Rancho La Brea that Howard (1947) recognized as a larger<br />
temporal form of A. chrysaetos also do not approach the length<br />
of the Inglis specimens (Table 2). Howard (1932) noted that the<br />
Rancho La Brea eagle had relatively longer wings and shorter<br />
legs than did recent A chrysaetos, but with a larger series of recent<br />
skeletons she later found that the limb proportions of the