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1 December 2008 A New Species of Large, Terrestrial Caracara from Holocene Deposits in Southern Jamaica (Aves: Falconidae)
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A new species of caracara, Caracara tellustris, is described from cave deposits in the arid Portland Ridge area of southern Jamaica. It is characterized by great size and much reduced wings, and was probably almost completely terrestrial in habits if not even flightless. It was thus probably confined to the more arid southern areas of the island where open country would be compatible with a terrestrial mode of life.

In the modern avifauna of the West Indies, the falconid subfamily Caracarinae is represented only by the Crested Caracara (Caracara cheriway) found in Cuba and the Island of Pines. The Cuban birds do not differ from those of Florida and the species is believed to be a recent colonist from the mainland (Suárez and Olson 2001). Caracaras of the genera Caracara and Milvago were once much more widespread in the Antilles, however, as indicated in the fossil record (Olson 1976, Morgan 1994, Suárez and Olson 2001, 2003).

The crested caracaras, genus Caracara (formerly Polyborus, but see Banks and Dove 1992) are represented as fossils by two named species: C. creightoni Brodkorb (1959) from Pleistocene and probable Holocene deposits in Cuba and the Bahamas (Olson and Hilgartner 1982, Suárez and Olson 2001, 2003) and C. latebrosus Wetmore (1920) known only from two fragmentary wing bones from cave deposits in central Puerto Rico. Both species were about the size of the living C. cheriway, although C. creightoni was slightly smaller. A hitherto unpublished caracara of this size is indicated on Mona Island, between Puerto Rico and Hispaniola, by a single well preserved notarium (USNM uncataloged) from an underwater cave deposit. Whether this was the same as P. latebrosus of Puerto Rico can only be determined with the collection of additional material. So far there has been no fossil record of Caracara from Hispaniola but this may be simply an artifact of collecting.

Another possibly distinct species of Caracara is indicated by the distal end of a right tarsometatarsus from a cave deposit on Grand Cayman (Morgan 1994). This specimen (UF 172841) was from a large species, the size (Table 1) of large individuals of the Southern Caracara (C. plancus; for the separation of C. plancus from C. cheriway see Dove and Banks 1999). It may be anticipated that this species will be found in Cuba as well.Table 2

Table 1

Measurements (mm) of hindlimb elements of Caracara. Sequence in modern taxa is: range (mean). Data taken partly from Suárez and Olson (2001). Measurements in boldface are from the holotype of C. tellustris n. sp.


Table 2

Measurements (mm) of pectoral elements of Caracara. Sequence in modern taxa is: range (mean).


The diversity of West Indian caracaras was further increased by the discovery of an exceptional new species of even larger Caracara from the arid parts of southern Jamaica, an island whose modern raptor fauna is notably depauperate (Olson 2006). This species is certain to have been endemic to Jamaica, as its pectoral elements indicate that it had very weak powers of flight at best (Table 2).

Materials and Methods

Complete recent skeletons, unless otherwise noted, from the collections of the National Museum of Natural History, Smithsonian Institution (USNM): Phalcobaenus australis 490979, Caracara cheriway USNM 11679 (partial postcranial), 19670-71, 321805, 322338, 343845-46, 346402, 428041, 431612, 553229-30, Caracara plancus 18478, 345779-80, 490931, 614583-84, 630187. Fossil specimens: Caracara latebrosa AMNH 4921, holotypical proximal end of right carpometacarpus; AMNH 4987, paratypical proximal end of right ulna. Caracara sp. UF 172841, distal end of right tarsometatarsus, Grand Cayman. Measurements were taken with digital calipers to the nearest 0.1 mm. In the photographs, the new fossil species is compared with large individuals of C. plancus, which is larger than C. cheriway, in order to emphasize the larger size of the Jamaican bird.


Class Aves

Family Falconidae

Genus Caracara Merrem, 1826

The Jamaican bird agrees in all general aspects with Caracara. The tarsometatarsus is much more slender and elongate than in Phalcobaenus (Figs. 1Figure 23) or in the much smaller Ibycter in which the tarsometatarsus is likewise short and robust. The tarsometatarsus of Daptrius and Milvago, which are probably best considered congeneric, may be difficult to separate on qualitative characters, as those previously thought to distinguish the two (Campbell 1979, Suárez and Olson 2003) appear to have been compromised by certain fossil material from Peru (W. Suárez and S. Olson unpubl. data). Nonetheless, the Jamaican bird is so large that it is unlikely to have been derived from any of the small, delicate species of Daptrius/Milvago.

Figure 1

Right tarsometatarsi of caracaras in anterior view. A, Phalcobaenus australis USNM 490979; B, Caracara tellustris, new species, holotype USNM 535727; C, C. plancus USNM 490931. Scale  =  2 cm.


Figure 2

Right tarsometatarsi of caracaras in posterior view. A, Phalcobaenus australis USNM 490979; B, Caracara tellustris, new species, USNM 535727; C, C. plancus USNM 490931. Scale  =  2 cm.


Figure 3

Right tarsometatarsi of caracaras in medial view. A, Phalcobaenus australis USNM 490979; B, Caracara tellustris, new species, USNM 535727; C, C. plancus USNM 490931. Scale  =  2 cm.


Caracara tellustris, new species

Figs. 1Figure 2Figure 3Figure 45

Figure 4

Left humeri of Caracara (A, B, E, F, anconal view; C, D, palmar view). A, C, F, C. plancus USNM 490931; B, D, C. tellustris, new species, USNM 535726; E, C. telluris, new species, USNM 535730. Scale  =  2 cm.


Figure 5

Right coracoids (A, B, ventral view; C, D, dorsal view) and pedal phalanx 1 of digit I in dorsal view (E, F) of Caracara. A, C, F, C. plancus USNM 490931; B, D, C. telluris, new species, USNM 535725; E, C. tellustris, new species, USNM 535729. Scale  =  2 cm.



Complete right tarsometatarsus USNM 535727 (Figs. 1Figure 23). Collected in 1995 by R.D.E. MacPhee and D.A. McFarlane.

Type Locality

Jamaica, Clarendon Parish, south coast of Portland Ridge, Jackson's Bay cave system, Skeleton Cave, Pit 1 down to 70 cm (see McFarlane et al. 2002).


Radiocarbon ages from various depths and parts of Skeleton Cave were all Holocene in age ranging from 1870 ± 50 before present to 6410 ± 110 BP at the deepest level (McFarlane et al. 2002).

Measurements (mm) of Holotype

See Table 1. Additional measurements, with paratype USNM 535728 in parentheses: length of calcaneal ridge of hypotarsus 17.9 (19.4); width and depth of middle trochlea 7.4 × 9.4 (damaged in paratype).


Skeleton Cave, Map Room: left humerus USNM 535726. Lloyd's Cave, Pit #1, Mantrap Entrance: right coracoid USNM 535725. Drum Cave, surface contents: proximal third of left humerus USNM 535723; shaft of right tibiotarsus. Jackson's Bay cave system, exact cave uncertain: distal half of right humerus USNM 535730; right tarsometatarsus USNM 535728; left pedal phalanx 1 of digit I USNM 535729.

Measurements (mm) of Paratypes

See Table 1.


L. tellustris, of the earth, from tellus, telluris, earth, land; in reference to the terrestrial habits and poor, or nonexistent, flying ability of the species.


A species of Caracara with hindlimb elements larger than in any other member of the genus or of the rest of the subfamily Caracarinae, whereas the pectoral elements are small in relation to body size and weakly developed, indicating extremely weak powers of flight or even flightlessness.


Except for larger size and more robust shaft, the tarsometatarsus resembles that of C. plancus although the scar for M. tibialis anticus is notably shorter and wider and has a flat rather than rounded surface, the scar for the hallux faces medially rather than posteriorly, and the wing of the inner trochlea is decidedly longer, narrower, and more distinctly set off from the rest of the trochlea. The large size of phalanx 1 of the hind toe (Fig. 5E) indicates that the foot was correspondingly large as well.

Although the coracoid falls within the range of C. plancus in length, the shaft is much narrower and the overall aspect is weak and feeble by comparison (Fig. 5B, D). Given the large size of the hindlimb, the humerus is small (Fig. 4B, D, E). The pectoral crest appears to have been greatly reduced and was rotated toward the palmar surface of the shaft, both of which are characters associated with flightlessness (Olson and Steadman 1979). The crest also extends farther distally than in C. plancus. The distal end of the humerus is less expanded than in C. plancus but the brachial depression is larger and much deeper, which is also associated with flightlessness. It may seem counterintuitive that M. brachialis almost always appears to be better developed in flightless birds but this can be explained by the fact that this muscle is important in keeping the wing folded, which is of much greater importance to a bird that does not use the wing for flight. The small size of the humerus in C. tellustris is demonstrated by the ratio of its length to the length of the tarsometatarsus, the mean ratios being: C. creightoni, 1.23; C. cheriway, 1.19; C. plancus, 1.24; and C. tellustris, 1.00. Thus, the humerus in typical caracaras is about 20% longer than the tarsometarsus, whereas in C. tellustris these elements are the same length.


Even with nearly complete skeletal material it is often difficult to predict from morphology whether a bird with reduced pectoral girdle and appendages would have been completely flightless. Caracara tellustris would have had at best very reduced powers of flight and probably led a nearly completely terrestrial existence, both foraging and dispersing on foot.

The habitat of C. tellustris was likely very restricted because such a large terrestrial avian predator could probably only function effectively in relatively open habitats. The vegetation of most of Jamaica prior to human settlement would have been closed forest or dense scrub (Asprey and Robbins 1953). Open habitats could probably have developed only in the drier southern parts of the island, and the caves in which the bones of C. tellustris were found are situated nearly at the southern tip of the island (McFarlane et al. 2002, Olson 2006). The most suitable habitat type would probably have been what Asprey and Robbins (1953) defined as thorn scrub, which is dominated by mimosoids such as Acacia and Prosopis. Thorn scrub is developed on alluvial sediments, which predominate in the southern part of the island. A littoral manifestation of thorn scrub is cactus scrub, in which cacti such as Stenocereus, Pilosocereus, and Opuntia are conspicuous. The region where this type of open scrub adjoins coastal flats and mangroves would probably have been ideal habitat for the caracara, but this habitat would have been of very limited extent, so that the population of C. tellustris was probably always quite small.

Prey of Caracara tellustris may have consisted of the wide variety of vertebrates, invertebrates, and carrion characteristic of the crested caracaras (e.g., Morrison 1996). Reptiles may have been an important component, as some 17 species of snakes and lizards occur on the Portland Peninsula (Schwartz and Henderson 1991), of which such ground-dwelling species as the skink (Mabuya spp.), teiids (Ameiva spp. and Celestus spp.), and young iguanas (Cyclura spp.), would have been paramount. In coastal areas, fiddler crabs (Uca spp.), of which there are six species in Jamaica, all occurring on the southern coast (Barnwell 1986), may have been a ready source of food.

As on most oceanic islands, extinction of the Jamaican caracara may have been a result of human interference of some kind. The small population of caracaras in the inhospitable hot, arid Portland Peninsula may have survived into the historic period only to be exterminated by introduced predatory mammals before its presence could be noted by naturalists. Also, the greatest changes in vegetation cover appear to have been effected following European settlement and agricultural expansion in the 1600s (Asprey and Robbins 1953).


I am first of all most grateful to Ross D.E. MacPhee and Donald A. McFarlane for collecting the fossil material of the new species and making it available and for their comments on the manuscript and much other shared information. Gary Graves also provided helpful comments. For lending holotypes of fossil caracaras I am indebted to the authorities of the American Museum of Natural History, New York (AMNH), and the Florida Museum of Natural History, Gainesville (UF). The photographs are by John Steiner, Smithsonian Photographic Services and the plates were composed by Brian Schmidt, Division of Birds.

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Storrs L. Olson "A New Species of Large, Terrestrial Caracara from Holocene Deposits in Southern Jamaica (Aves: Falconidae)," Journal of Raptor Research 42(4), 265-272, (1 December 2008).
Received: 25 March 2008; Accepted: 1 August 2008; Published: 1 December 2008

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