Temporal range: Late Eocene
|Zygorhiza kochii skeleton, Smithsonian National Museum of Natural History|
Zygorhiza ("Yoke-Root") is an extinct genus of basilosaurid early whale known from the Late Eocene (Priabonian, 38–34 Ma) of Louisiana, Alabama, and Mississippi, United States, and the Bortonian (43–37 Ma on the New Zealand geologic time scale) to the late Eocene of New Zealand ( ). Specimens reported from Europe are considered Dorudontinae incertae sedis.
In the late 19th century there was a debate whether large and small specimens of Zeuglodon brachyspondylus (=Basilosaurus, but the species is now considered a nomen nudum) were separate species or not. Hoping to clarify things, Stromer 1903 proposed using Z. brachyspondylus exclusively for large fossils and created the subspecies Z. brachyspondylus minor for the small specimens which had previously been synonymized with Dorudon serratus. True 1908 proposed the genus Zygorhiza for the subspecies. Adopting True's generic name, Kellogg 1936 synonymized this subspecies with Basilosaurus kochii and Zeuglodon hydrachus (better known as "Dr Albert Koch's Hydrarchos", see Pontogeneus) and half a dozen other combinations and placed them in the species Zygorhiza kochii.
Seeley 1876 named and described the species Zeuglodon wanklyni based on a skull that is friend Dr. Arthur Wanklyn had found in the Barton Clays in southern England. This skull, however, was never deposited at the British Museum of Natural History and has not been since Seeley described it. Kellogg 1936, nevertheless, recombined it as Zygorhiza wanklyni and referred a posterior cervical vertebra from the same location to it. Uhen 1998 declared it nomen nudum.
Köhler & Fordyce 1997 described an incomplete skull, four vertebrae, two teeth, and small fragments in early Bartonian sediments in New Zealand which they tentatively identified as Zygorhiza sp.. This is the oldest known Dorudontinae and the oldest known cetacean from the Southern Hemisphere
In the U.S., Zygorhiza is known from the Gulf Coast, whilst Dorudon is known from southeastern Atlantic Coast. Outside North America, Zygorhiza has only been reliably identified in New Zealand, whereas Dorudon only in Egypt. It is possible that these non-overlapping distributions indicate differences in habitat preferences.
Like other dorundontines, Zygorhiza had a body similar to modern cetaceans with flipper-like forelimbs, rudimentary hind limbs, a vertebral column adapted for oscillatory swimming, and a tail fluke.
Marino et al. 2000 estimated the adult body mass for Zygorhiza to 3,351 kg (7,388 lb) based on an estimated body length of 520 cm (200 in). Using CT scans, they estimated the brain weight to 738.2 g (26.04 oz), resulting in a EQ value of 0.26 (compared to 0.54 for a modern cetacean such as Cuvier's beaked whale.)
The permanent dental formula for Zygorhiza is 18.104.22.168, the deciduous dental formula is 3.1.4. The cingula at the base of the tooth crowns on P2–4 are strongly developed but do not meet on the medial side. P2, the largest upper tooth, has four accessory denticles on the anterior and posterior cutting edges. P3–M2 form a closed series. P2–M2 have two widely separated roots, accessory denticles on the anterior and posterior cutting edges, and anastomosing striae on the enamel. P1 is caniniform with a single root. P2–4 have laterally compressed crowns and accessory denticles on the anterior and posterior cutting edges. P4 is the largest lower tooth. M1–3 have accessory denticles on the posterior cutting edges. P2–3 are two-rooted. Outside the upper one-rooted teeth and inside the upper two-rooted teeth there are pits for reception of the lower teeth.
Zygorhiza (and Dorudon) replaced their upper and lower deciduous first premolars with permanent teeth. This is very unusual in modern mammals and contrasts to extant toothed whales that only develop a single set of teeth. It might indicate that Zygorhiza represents a stage in archaeocete evolution where skeletal maturation was delayed like in modern cetaceans. Zygorhiza differs from all other dorudontines in the presence of well-developed cuspules on the cingula of the upper premolars.
The skull is elongated with a narrow rostrum and a flattened forehead; the premaxillae are laterally convex. The high sagittal crest is flanked by two large temporal fossae, resulting in a narrow intertemporal region.
The hyoid apparatus consists of a small, central, and hexagonal basihyoid bone. From this bone project a pair of thyrohyoid bones (homologous with the greater cornua in humans) that are slightly expanded anteriorly and tapper off posteriorly, and another pair of slender and elongated bones, the epihyoid and stylohyoid bones.
The vertebral formula is 7 cervicals, 15 thoracics, probably 13 lumbars, 2 sacrals, and at least 21 caudals. The centra of the posterior thoracic, lumbar, sacral, and anterior caudal are slightly elongated. The centra of the cervicals are compressed and the flexibility in the neck is limited by the interlocked lateral processes. The atlas has a hypapophysial (ventral) process. The axis a small odontoid (tooth-like) process, short and narrow transverse processes, and an elongated neural spine.
- Zygohriza in the Paleobiology Database. Retrieved July 2013
- Uhen 2009, p. 93
- Johnston, John E. "Fossil Whale: State Fossil of Mississippi" (PDF). Retrieved April 2013.
- "Indoor Exhibits Map: Stories in Stone". Mississippi Museum of Natural Science. Retrieved July 2013.
A showcase for some of Mississippi's most important fossils, including ocean-dwelling trilobits, meat-eating dinosaurs, and Zygorhiza, the early whale known by his friends as "Ziggy".
- True 1908, p. 67
- True 1908, p. 78
- Kellogg 1936, pp. 101–102
- Kellogg 1936, pp. 174–175
- Basilosauridae: Taxonomic history in the Paleobiology Database. Retrieved September 2013.
- Köhler & Fordyce 1997, Abstract
- Uhen 2006
- Gray et al. 2007, p. 639
- Marino et al. 2000, pp. 87, 90
- Kellogg 1936, pp. 100–101
- Uhen 2000, Abstract
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- "Kellogg Illustration Gallery, including 37 illustrations of Zygorhiza from Kellogg 1936.". Smithsonian NMNH. Retrieved September 2013.