How did a hoofed land mammal become the largest animal on the planet, able to dive to depths of hundreds of metres, to echolocate in the dark or to sing across thousands of kilometres? The evolution of the cetaceans is one of the best documented transitions in the history of life. In some fifty million years, a small semi-aquatic artiodactyl wholly reinvented its anatomy in order to take to the oceans. This page retraces that history, stage by stage, from the key fossils and the molecular evidence, and points to our detailed pages on the fossil ancestors of the cetaceans and the terrestrial ancestor of the cetaceans.
Did you know? The closest living relative of the cetaceans is… the hippopotamus. The two lineages diverged about 53 to 55 million years ago (molecular estimate). Together they form the clade Whippomorpha. This relationship, long a surprising one for palaeontologists, has been confirmed almost irrefutably by genetics.
For a long time the origin of the cetaceans seemed a puzzle: how could these fully water-adapted marine giants be connected to a land ancestor? It is now known that the cetaceans descend from terrestrial ungulates, and more precisely from the artiodactyl lineage (the large group of cattle, pigs, deer, camels and hippopotamuses). Two entirely independent lines of evidence converge on that conclusion.
The most decisive genetic evidence comes from SINE retrotransposons: these short DNA sequences insert themselves at random into the genome and are passed on there from generation to generation. The work of Shimamura, Nikaido and their colleagues showed that cetaceans and hippopotamuses share SINE insertions at the same positions in the genome. Since the probability of such an insertion occurring twice independently at the same site is vanishingly small, these markers constitute an almost irrefutable signature of common ancestry. They define the clade Whippomorpha (hippopotamuses plus cetaceans).
The genetic data and the fossils for a time appeared to contradict one another, until the discovery, in protocetids such as Rodhocetus and Artiocetus, of a characteristic ankle bone: the double-pulley astragalus, described by Gingerich and his colleagues in 2001. This form of astragalus, with its two pulley-grooved articular surfaces, is an exclusive signature of the artiodactyls. Finding it in early cetaceans finally reconciled morphology and genetics: the cetaceans are indeed aquatic artiodactyls, and not the descendants of the carnivorous mesonychians as had first been supposed. To explore the relationships among the living species further, see our interactive phylogeny of the cetaceans.
This timeline is ordered by evolutionary and ecological stage, not strictly by date: Indohyus (~48 Ma) is an artiodactyl cousin contemporary with the lineage, not an ancestor older than Pakicetus (~50 Ma).
Indohyus, a small artiodactyl of the raoellid family (the size of a fox), is today regarded as one of the closest fossil relatives of the cetaceans on the terrestrial side. Described as early as the 1970s by A. Ranga Rao, it was Hans Thewissen who brought out its importance in 2007 (Nature): its ear already showed the structure characteristic of cetaceans, and its dense bones (osteosclerosis) indicated a semi-aquatic way of life, probably walking on the bottom as the hippopotamus does today. Indohyus was not a direct ancestor, but it illustrates what the close artiodactyl relative from which the cetacean lineage diverged looked like.
Discovered in present-day Pakistan, Pakicetus (~50 Ma, with deposits dated at around 48.5 Ma) is one of the oldest recognised cetaceans and the best documented at this stage. Contrary to a widespread image, it was not a “sea dog”: it was a four-legged hoofed mammal the size of a wolf (~1 to 2 m), with long functional legs. It lived beside watercourses and is today regarded as semi-aquatic and tied to fresh water: Thewissen’s reconstruction (2001) describes it as “no more amphibious than a tapir”, that is, able to move about on land but strongly associated with shallow aquatic habitats. Its diagnostic character is acoustic: the tympanic bulla formed from the ectotympanic bone alone, and the involucrum, middle ear structures peculiar to cetaceans. But Pakicetus could not yet hear well underwater: it lacked the fatty pad in the jaw that carries waterborne sound in modern cetaceans, and it picked up sound through the external auditory canal, like a land mammal.
Ambulocetus natans (“the walking whale that swims”) is one of the most emblematic fossils of this transition. With its short legs, its webbed hands and feet, its elongated snout and its body of about 3 metres, it suggests an amphibious predator lying in wait in shallow water, an ambush hunt comparable, in ecological terms, to that of a crocodile. For swimming, on the other hand, it is compared rather to a large otter: it propelled itself by dorsoventral undulations of the back and by powerful hind feet, and not by crocodile-like lateral movements.
Rodhocetus, a protocetid of the Lutetian (~46-47 Ma), marks a major step towards marine life: reduced hind limbs, nostrils set further back, streamlined body. It is also in this animal that the double-pulley astragalus which confirmed artiodactyl ancestry was identified. The idea that it already possessed the “locomotor signature” of modern cetaceans has, however, now been revised: Gingerich (2003) considers that Rodhocetus probably had no tail fluke and swam mainly at the surface by alternating beats of the hind feet, the tail serving above all as a rudder, a mode close to that of the desman or the otter. True propulsion by undulation of the tail would appear later, in the basilosaurids.
Described as early as the 19th century, Basilosaurus is a wholly marine cetacean, very elongated, 15 to 20 metres long, without functional hind limbs but retaining tiny vestigial legs. Its relative Dorudon, more compact (~5 m), is probably more representative of the lineage that gave rise to the present-day cetaceans. The basilosaurids propelled themselves with the tail and very probably had a horizontal tail fluke, an inference drawn from the proportions of their caudal vertebrae, since the fluke, having no bone, does not fossilise. The exact swimming mode of Basilosaurus, whose body is particularly serpentine, remains debated; recent analyses (Gingerich, Uhen) favour essentially dorsoventral undulations rather than lateral ones.
Towards the end of the Eocene, the Neoceti lineage divides into two groups with distinct ecological trajectories. Molecular estimates place this divergence about 34 to 39 million years ago (central value ~37 Ma according to Steeman et al., 2009), while the fossil record documents it from about 34 Ma onwards: the Oligocene record does not always support a radiation as early as the molecular clocks indicate, and this remains a matter of debate.
This divergence allowed the two groups to occupy complementary ecological niches (see the difference between whale, sperm whale and dolphin).
Baleen did not appear all at once. The oldest known mysticetes still had teeth: Mystacodon, Coronodon and Janjucetus were toothed mysticetes without baleen, while Aetiocetus (Oligocene) shows both teeth and indications of baleen, an intermediate stage in the shift to filter feeding. In parallel, the first odontocetes capable of echolocation appear in the Oligocene. Acoustic specialisation and filter feeding therefore came into place gradually, and not instantaneously.
The superfamily Physeteroidea diverges from the rest of the odontocetes about 25 million years ago. It brings together two living families: the Physeteridae (a single living species, the sperm whale, Physeter macrocephalus) and the Kogiidae, which differentiate later and comprise the pygmy sperm whale (Kogia breviceps) and the dwarf sperm whale (Kogia sima). Beware of a frequent error: the two Kogia are not Physeteridae but Kogiidae; it is the superfamily Physeteroidea that unites them with the sperm whale.
The oceanic dolphins (Delphinidae) diversify, giving the most numerous family of living cetaceans: common bottlenose dolphin, common dolphin, killer whale, pilot whale, Risso’s dolphin… This is also the period of expansion of the porpoises and the river dolphins.
The blue whale (Balaenoptera musculus) is the largest animal known from any period. Its gigantism belongs to a shift in the evolutionary regime of body size in the Plio-Pleistocene, dated to about 4.5 million years ago (Slater, Goldbogen & Pyenson, 2017). This shift is linked to the seasonal intensification of cold-water upwelling, which concentrates krill into dense swarms that can be exploited by bulk filter feeding. The extreme gigantism of the rorquals is above all Pleistocene: speaking of the blue whale “appearing” at 4 Ma is therefore a convenient but approximate shorthand.
Evolution leaves anatomical traces that are visible in the bodies of modern cetaceans, so many clues to their terrestrial past:
| Period | Key species | Characteristic |
|---|---|---|
| ~48 Ma | Indohyus | Semi-aquatic artiodactyl, close relative of the cetaceans |
| ~50 Ma | Pakicetus | Hoofed quadruped, ear already “cetacean” |
| ~49 Ma | Ambulocetus | Amphibious, webbed feet, ambush hunting |
| ~47 Ma | Rodhocetus | Semi-aquatic, still swimming with the feet; artiodactyl astragalus |
| ~40 Ma | Basilosaurus / Dorudon | Fully marine, up to ~20 m, inferred fluke |
| ~34-39 Ma | Split of the lineages | Mysticetes vs odontocetes (Neoceti) |
| ~25 Ma | Physeteroidea | Sperm whale lineage (Physeteridae + Kogiidae) |
| ~10 Ma | Delphinidae | Diversification of the oceanic dolphins |
| ~4.5 Ma | Balaenoptera musculus | Shift towards rorqual gigantism |
Ma = million years before present
Did you know? Cetacean taxonomy is still very much alive. Rice’s whale (Balaenoptera ricei), endemic to the Gulf of Mexico, was described only in 2021, after long being confused with the Bryde’s whale complex (Balaenoptera edeni). With an estimated population of some fifty individuals, it is listed as Critically Endangered by the IUCN: evidence that new species of large cetaceans can still be recognised today.
The reference list of the Committee on Taxonomy of the Society for Marine Mammalogy (SMM), updated regularly, recognises about 94 living cetacean species, one of them possibly extinct, the baiji (Lipotes vexillifer, family Lipotidae), listed by the IUCN as “Critically Endangered (possibly extinct)”. They divide into 15 mysticetes (baleen whales, 4 families) and 79 odontocetes (toothed whales, 10 families). This figure changes regularly with taxonomic revisions: newly described species, lumping or splitting of species. For the detailed list by family, see our pages on the mysticetes and the odontocetes, as well as the IUCN conservation statuses.
Several cases show that the classification of the cetaceans is not fixed. The position of the pygmy right whale (Caperea marginata) is debated: the SMM places it in the Neobalaenidae, but a hypothesis founded on fossils (Fordyce & Marx, 2012) attaches it to the Cetotheriidae, a family long held to be extinct, in which case Caperea would be its only “living fossil”. Likewise, the Bryde’s whale complex remains debated: Balaenoptera edeni brings together two subspecies (edeni and brydei), and Rice’s whale (Balaenoptera ricei), long confused with that complex, was validated as a distinct species only in 2021. Finally, the Ganges and Indus river dolphins (genus Platanista), long grouped into a single species, are now recognised as two distinct species (Platanista gangetica and Platanista minor) following the work of Braulik and colleagues (2021). On the points that remain unsettled, the scientific approach is to set out the debate rather than to settle it arbitrarily.
An exemplary evolution
The history of the cetaceans is one of the best known examples of a documented macroevolutionary transition. The fossil sequence, from Indohyus to Basilosaurus, is dense enough, and each stage distinct enough, to reconstruct the passage from land to sea in detail, in agreement with the molecular evidence.
The cetaceans descend from terrestrial artiodactyls (the group of even-toed ungulates). Their closest living relative is the hippopotamus: together they form the clade Whippomorpha. This relationship is established by the shared SINE genetic markers and by the double-pulley astragalus of fossil cetaceans.
About 10 million years: from Pakicetus (~50 Ma), semi-aquatic and tied to fresh water, to Basilosaurus and Dorudon (~40 Ma), fully marine. Modern cetaceans then went on evolving for nearly 40 million years more.
At the end of the Eocene, about 34 to 39 million years ago (molecular estimate ~37 Ma, Steeman et al., 2009; first fossil indications at around 34 Ma). The two groups then independently developed baleen filter feeding (mysticetes) and echolocation (odontocetes), both of which appeared gradually during the Oligocene.
About 94 living species according to the reference list of the Society for Marine Mammalogy (updated regularly), one of them possibly extinct (the baiji): 15 mysticetes (4 families) and 79 odontocetes (10 families).
No, not entirely. These small pelvic bones, a terrestrial legacy, are today regarded as functional: they anchor the reproductive musculature and are under sexual selection (Dines et al., 2014). They have been reduced and reassigned rather than simply kept as useless relics.
