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A Middle Jurassic Malagasy mammaliaform known from lower teeth in a jaw fragment. Its tribosphenic-like construction bears on competing hypotheses for the origin of tribospheny. ^[ref]

A Late Jurassic avian-lineage theropod dinosaur outside the living-bird crown group under standard relationships.

A Middle Jurassic mammaliaform with aquatic adaptations and preserved integument. The fossil supplies a minimum occurrence for a fur-bearing covering, not the exact origin date of endothermy. ^[ref]

An Early Jurassic mammaliaform with a small skull documenting changes in the jaw, ear attachment and braincase. ^[ref]

Mammalian endothermy probably emerged through several interacting changes along the synapsid stem, and its precise onset remains disputed because the fossil proxies measure different aspects of physiology. Endothermy concerns substantial metabolic heat production; homeothermy concerns relatively constant body temperature. A large animal can have relatively stable temperature without a mammalian metabolic rate, while an endothermic animal can display heterothermy. These distinctions prevent a single temperature estimate or anatomical character from being treated as a complete diagnosis.

The physiological problem is a heat balance. In a deliberately simplified steady-state model:where $M$ is metabolic energy turnover, $W$ external work, $G$ effective thermal conductance of an animal, $T_b,T_a$ body and ambient temperature, and $E$ evaporative heat loss. Maintaining a warm body in a cool environment can involve increased metabolism, reduced conductance, behaviour, or a combination. For example, $G=0.1\mathrm{W}{\mathrm{K}}^{-1}$ and a $20\mathrm{K}$ difference imply $2\mathrm{W}$ of non-evaporative heat loss in this illustrative model. The numbers are not a reconstruction of a fossil animal.

Along the synapsid lineage, increased sustained activity would require coordinated oxygen uptake, transport and use, greater food processing and sufficient energy assimilation. More effective locomotor construction, ventilation and circulation could support greater aerobic capacity, while insulation would reduce the cost of retaining the resulting heat. Shivering thermogenesis and later forms of non-shivering thermogenesis can contribute in living mammals. Brown adipose tissue in many living placental mammals cannot simply be assigned to early therapsids; a modern mechanism need not have been the ancestral one. Similarly, an expanded secondary palate or an altered limb posture is compatible with increased performance but is not a direct measurement of resting metabolism.

The time sequence must be reconstructed from several lines of evidence. Early synapsids lack the complete modern mammalian package, whereas various therapsids and cynodonts show changes in growth, feeding and respiratory anatomy before the mammalian crown radiation. Rapidly deposited fibrolamellar bone supports rapid growth, but fast-growing ectotherms and the influence of size and environment prevent a unique inference of endothermy. Growth interruptions can reflect seasonality or resource shortage rather than a categorical physiological boundary. Nasal structures interpreted as respiratory nasal turbinates could reduce water and heat loss during high ventilation, but identifying their precise form and separating respiratory from olfactory roles in fossils is difficult.

Preserved hair supplies direct evidence of insulation in some later fossils. Castorocauda, a Middle Jurassic mammaliaform, preserves integument alongside an aquatic anatomical specialization. ^[ref] This establishes that a fur-bearing covering existed by that time, not when insulation first evolved or whether its original function was thermal. Sensory and protective functions can precede elaboration for heat conservation. Direct preservation is particularly valuable, but its late appearance in the sampled record is not proof of biological absence in older lineages.

Stable isotope analysis has suggested earlier elevated thermometabolism. Comparing oxygen-isotope compositions of therapsid apatite with those of coexisting tetrapods, one study inferred differences in physiology and proposed elevated thermometabolism in several Permo-Triassic therapsid groups. ^[ref] The comparison is stronger than analysing one isolated animal because coexisting taxa constrain aspects of the environment. Nevertheless, body water, drinking source, habitat, evaporation and diagenesis affect the isotopic signal. The proposed middle-to-late Permian origin is an interpretation using a physiological framework, not a thermometer reading of an observed living cynodont.

A contrasting biomechanical approach uses the temperature dependence of endolymph properties and the dimensions of the semicircular canals. Calibration against living animals and application to fossil inner ears supported a relatively abrupt transition around 233 million years ago in the Late Triassic, near the origin of mammaliamorphs. ^[ref] This offers a quantitative prediction from a different anatomical system. However, body size, activity, reconstruction and the adequacy of the living calibration remain relevant. A change in a temperature-sensitive inner-ear proxy need not coincide exactly with the first increment in metabolic heat production or the first insulating covering. The disagreement with earlier isotope-based interpretations should therefore be tested, rather than erased by choosing the preferred date.

There are several plausible selective explanations. The aerobic capacity hypothesis proposes that selection for sustained locomotor performance raised maximum oxygen consumption, with elevated resting metabolism and heat production linked to that change. Comparative measurements of resting and maximum oxygen use underpin this proposal. ^[ref] A major issue is the strength and evolutionary direction of the relationship: high resting expenditure is expensive, and an association among living species does not prove which change led historically. Selection for thermal independence, nocturnal activity or performance in fluctuating climates provides related benefits, but “the climate became colder” is not sufficient unless the energetic costs and available food are considered.

A parental care hypothesis instead emphasizes selection for controlling the developmental environment and supplying offspring. Improved provisioning endurance and more stable incubation or offspring temperatures could favour increased metabolic capacity and heat retention. ^[ref] This gives concrete reproductive benefits that might offset energetic costs, while remaining a hypothesis about historical selective circumstances. The evidence required includes relationships among care, thermal performance and reproductive success, not merely the fact that living mammals both care for young and are endothermic. Activity, parental investment, insulation and environmental variability could reinforce one another, so the explanations need not be mutually exclusive.

The most secure account is a mosaic physiological transition with increasingly effective energy supply, heat production and heat retention. A Late Triassic onset of a more fully mammalian condition is a specific supported hypothesis, while earlier therapsid evidence indicates that parts of the transition may be older. fossil anatomy and chemistry constrain when particular features existed; the selective reasons require functional and comparative tests and remain less directly observable.

The frog skeleton evolved through mosaic evolution: reorganization of the head and pelvis preceded completion of the compact, tailless, long-limbed jumping apparatus. Its principal transformations are shortening and stiffening of the axial skeleton, conversion of the posterior body into a sacrum–pelvis–urostyle system, and specialization of the appendicular skeleton for propulsion and landing. These are connected mechanically, but need not have evolved simultaneously or initially served the same function.

In the derived adult frog, the trunk is short, most species having eight or nine presacral vertebrae, and the ribs are strongly reduced or absent. The adult tail no longer consists of a long freely jointed series. Instead, the urostyle forms a posterior axial rod from caudal vertebral and associated developmental components. This increases the integration of the posterior body with the pelvic girdle. The ilium has an elongated, anteriorly directed shaft, placing much of the pelvic apparatus posterior to its sacral connection. Changes in the sacroiliac joint and adjacent musculature permit transmission of bilateral hindlimb thrust to the trunk. The urostyle is therefore more than a tail that simply shrank: it is part of a reorganized force-transmission system.

The limbs change in both proportion and construction. Elongate hindlimbs increase the possible extension stroke, and elongated proximal ankle elements, the tibiale and fibulare, add another effective segment to the propulsive chain. Union of tibia and fibula into a tibiofibula and of radius bone and ulna into a radioulna stiffens the lower limb segments. The forelimbs and pectoral girdle participate in support and absorption of landing forces, while the frog head is typically broad, short and flattened, with reduction and fusion of cranial elements, including integration of frontal and parietal components into a frontoparietal bone. These are generalizations about the characteristic skeleton, not a claim that every living frog is an obligate jumper: swimming, burrowing, climbing and walking lineages modify the inherited apparatus.

The decisive stem example is Triadobatrachus massinoti, from the Early Triassic of Madagascar, about 250 million years ago. It belongs to the frog total group, Salientia, outside crown Anura. Its phylogenetic importance is the association of recognizable frog-lineage features with retained ancestral construction. An anteriorly elongated ilium and frog-like cranial organization were already present, while a short series of separate caudal vertebrae persisted. The forearm and lower-leg pairs were not united into the modern radioulna and tibiofibula, and the hindlimbs lacked the full proportional specialization of powerful living jumpers. Thus pelvic reorganization did not require that all the later limb and tail modifications had already evolved.

The 2016 micro-computed tomography redescription is especially important because it revises the evidence rather than merely repeating an iconic reconstruction. It recognized 15 presacral vertebrae, with an atlas vertebra–axis vertebra complex, replacing the traditional interpretation of 14 with a divided atlas. Its trunk was therefore substantially less abbreviated in vertebral count than that of a typical living frog. Reconstructions under alternative amphibian relationships suggested that some proportional trunk reduction may already have occurred before the frog–salamander split, preceding the iliac elongation and tail shortening seen in this fossil. That inference depends on the comparative tree and model; vertebral number and actual trunk proportions are different characters. A count alone cannot demonstrate exactly how flexibly the animal moved.^[ref]

Locomotor inference requires an additional test. In 2016, Andrés I. Lires and colleagues compared major limb-bone lengths across 188 living limbed amphibians and lizards, relating their proportions to observed locomotor categories while considering shared ancestry. Triadobatrachus massinoti was better supported as using salamander-like lateral undulatory locomotion than as a specialized jumper. This is evidence against assuming that each frog-like skeletal feature originated as an adaptation for saltation. The limitations are that bone proportions are proxies for performance, living comparison sets may omit extinct combinations, and soft tissues and direct behaviour remain unknown. Failure to support specialized jumping does not exclude every short hop or vigorous hindlimb movement.^[ref]

Comparison with Prosalirus bitis, from the Early Jurassic, provides a later anatomical checkpoint. Its caudopelvic construction includes a urostyle, rod-like iliac organization and elongate hindlimbs, and was interpreted as supporting jumping through changes in pelvic orientation and iliosacral mobility. This comparison reinforces a sequence in which early frog-lineage pelvic and cranial modifications preceded completion of the more specialized locomotor system. It does not turn the named fossils into a direct ancestor–descendant chain, nor require every phylogenetic character to have followed exactly the same history in every branch.^[ref]

Triadobatrachus massinoti separates frog ancestry from fully developed frog jumping. It documents a combination that comparison of living frogs and salamanders alone could not predict reliably. The appropriate evolutionary explanation allows early changes in body support or movement to become exaptations for later saltation, followed by stronger specialization of the limbs and caudopelvic apparatus. Its retained tail and incompletely fused appendicular elements demonstrate staged assembly, while the revised vertebral interpretation shows why the ordering must remain anchored to observed anatomy.

cetaceans illustrate a sequence of inherited mammalian features, terrestrial specializations and subsequent aquatic transformations, followed by divergence in feeding and sensory anatomy. This is a branching phylogenetic tree, not a procession of named fossils that can all be identified as direct ancestors. Here Cetacea includes living whales, dolphins and porpoises; mammals means the crown group containing living monotremes and therians, whereas mammaliaforms also includes close extinct relatives outside that crown group. Dates below are approximate millions of years ago, abbreviated Ma.

The starting condition is a terrestrial, non-mammaliaform cynodont, itself a therapsid within Synapsida. Along the mammalian stem group, enlargement of the dentary and reduction of the other lower-jaw bones accompanied more differentiated teeth, increasingly precise dental occlusion and elaboration of a secondary palate. These changes belong to a feeding and respiratory complex: a larger tooth-bearing bone carries the mastication load, differentiated teeth process food, and a bony partition separates nasal and oral passages. They were acquired in a mosaic; neither a full modern mammalian jaw nor the aquatic body plan appeared at the initial divergence from other cynodonts.

Early mammaliaforms show how jaw support and hearing became reorganized. Morganucodon, around the Triassic–Jurassic transition and Early Jurassic, retained the old articular–quadrate jaw joint alongside a dentary–squamosal joint. In the mammalian condition the dentary–squamosal articulation supports the jaw, while the articular and quadrate correspond to the malleus and incus; the angular bone contributes to the ectotympanic. This is biological homology supported by comparative anatomy and biological development, not merely similarity in function. Hadrocodium, about 195 Ma, records further changes in jaw attachment and the braincase consistent with increased separation of mastication and hearing. Its tiny skull does not preserve an entire living-style ear apparatus; the reconstruction depends partly on bony attachment evidence. ^[ref]

The inherited mammalian package also includes diphyodonty, hair and lactation, although the latter two leave much poorer evidence in these particular fossils than do teeth and jaws. Precise adult dental occlusion is easier to maintain when repeated replacement ceases. The lineage subsequently passed through Theria, Eutheria and the ancestors of living placental mammals. These nested relationships matter: a Cretaceous eutherian is not automatically a member of the living placental crown group, and neither the first known fossil nor the date of a tooth innovation fixes the origin of an entire group.

The immediate terrestrial context of whale evolution is within Artiodactyla, broadly circumscribed to include Cetacea. Living hippopotamuses are the closest living relatives of cetaceans, not their ancestors. Some early whale teeth suggested relationships with extinct mesonychians, but dental resemblance alone was misleading. Early whale skeletons preserve the characteristic artiodactyl double-pulley astragalus, providing a powerful independent anatomical test of the relationship inferred from molecular evidence. The relevant comparison is the detailed construction of the ankle, not simply whether an animal has hooves or eats meat. ^{[ref] [ref]}

Early Eocene pakicetids, roughly 50 Ma, combine a largely terrestrial, weight-bearing skeleton with diagnostic whale ear-region anatomy, notably the thickened medial wall of the auditory bulla called the involucrum. Thus identification as a whale does not imply an obligately marine animal. Ambulocetus, roughly 48 Ma, has a different combination: robust limbs still useful around shore, large feet and an axial skeleton suited to substantial movement in water. Reconstruction of amphibious locomotion uses limb proportions, joint surfaces and vertebral anatomy together; it does not require assuming that its swimming exactly resembled an otter's. These are successive grades represented by branching relatives, not proof that a particular pakicetid gave birth to the known Ambulocetus specimen. ^[ref]

Middle Eocene protocetids further document reduction of terrestrial support and increasing commitment to swimming. Changes in the connection between pelvis and vertebral column, limb proportions and the position of external nostrils occurred in different combinations. The ankle of Rodhocetus is especially informative about ancestry even while other parts of its skeleton document aquatic specialization. It would be unjustified to draw a preserved tail fluke onto Rodhocetus: a reconstructed swimming mode must distinguish actual preserved anatomy from inferred soft parts. ^[ref]

Aquatic hearing changed alongside locomotion. Enlargement of the mandibular sound-reception region and changes in the middle ear support a transition towards receiving underwater sound through the lower jaw, with increasing acoustic separation of the ears from the skull. Early whale lineages display different intermediate combinations, so the presence of an involucrum alone does not imply a modern dolphin hearing system. Reconstructing soft sound-conducting tissues requires comparison with living anatomy; the fossil preserves their bony context rather than the entire pathway. ^[ref]

By the later Eocene, basilosaurids were fully aquatic. The forelimbs functioned as flippers, the vertebral column and tail supplied propulsion, and the hind limbs were far too small to support terrestrial walking. Nevertheless, the reduced limbs of Basilosaurus retain recognizable limb and foot elements. Loss of a locomotor role is not equivalent to absence of all function; reproductive or muscular roles are compatible with reduction, although a specific behaviour cannot be read directly from a bone. The transition therefore involved changing proportions and connections as well as losses. ^[ref]

Finally, the living branches acquired different specializations. Odontoceti retain teeth and evolved specialized sound production and echolocation; Mysticeti evolved baleen and lack functional adult teeth. fossil toothed mysticetes and degraded enamel-related genes show that modern toothlessness is derived. Palatal vascular features have been used to infer an intermediate combination of teeth and baleen, but such foramina do not preserve the baleen itself, and the exact sequence of feeding behaviours is less secure than the transition from toothed ancestry. ^[ref] The resulting history explains why a whale can have a mammalian jaw and reproductive system, an artiodactyl ancestry, a radically modified swimming skeleton, and a feeding apparatus that evolved after the aquatic transition. The strongest reconstruction combines nested anatomical characters with independently dated fossils, while treating soft-tissue and behavioural reconstructions as hypotheses.

Southern fossils have changed the geography, timing and anatomical character of mammaliaform evolution, while exposing how strongly a northern fossil record had shaped earlier expectations. Their importance is not that every southern lineage arose in the south. A dated occurrence establishes presence and a minimum age; an evolutionary origin requires an argument from phylogenetics and biogeography. Nor do modern continental outlines reproduce the connections of Gondwana.

A particularly consequential example is Ambondro mahabo, represented by a jaw fragment with lower teeth from Middle Jurassic Madagascar, approximately $167\pm 2$ Ma. The teeth possess a basined heel associated with the crushing component of tribosphenic molars, which combine shearing and crushing in a single occlusal system. Its age extended the then-known record of this dental construction substantially backwards and challenged a simple northern origin inferred from better-sampled northern localities. The material nevertheless consists of a very restricted part of the animal, and the matching upper dentition was not directly observed. Assigning the entire skeleton, physiology or reproductive mode from these teeth would go beyond the evidence. ^[ref]

The discovery also changed the character of the phylogenetic question. One hypothesis groups several southern forms in Australosphenida, associated with the ancestry of monotremes, and proposes that a tribosphenic-like construction arose independently of northern Boreosphenida, including therians. In that interpretation a highly functional tooth arrangement is convergent evolution, not a unique certificate of therian ancestry. A competing analysis supports a single origin of tribospheny and rearranges the relationships of the relevant southern taxa. ^{[ref] [ref]} The important lesson is not to declare one historical topology established by the striking tooth alone. The choice depends on which cusps and basins are judged instances of biological homology, character coding, inclusion of other anatomical regions, and the taxon sample. Nor does a Middle Jurassic tribosphenic tooth by itself date the split between living marsupials and placental mammals.

South American monotreme material further undermined the equation of present distribution with evolutionary birthplace. Early Paleocene Monotrematum, approximately 60–65 Ma, has teeth with affinities to the platypus lineage. Living monotremes are restricted to Australasia, but that restriction cannot be projected unchanged into the past. ^[ref] South America, Antarctica and Australia offered changing opportunities for connection, fragmentation and movement. A South American occurrence is compatible with a geographically extensive southern history; it does not uniquely establish the direction of dispersal or prove that Monotrematum was the direct ancestor of the living platypus. The distinction between a crown group and related members of its stem group is essential when attaching such fossils to divergence-time estimates.

Latest Cretaceous Madagascar has contributed more than isolated tooth surprises. The cranium of Vintana, around 70 Ma, supplied extensive new characters for the formerly tooth-dominated Gondwanatheria. Its robust feeding apparatus and unusual cranial combination permit tests of relationships and ecology that were unavailable from a few teeth. Yet a mosaic of familiar and unusual features is precisely the situation in which a single apparently diagnostic character can mislead. The placement of gondwanatherians therefore needs broad anatomical and taxonomic comparison, including other extinct groups, rather than assignment to a living order by superficial resemblance. ^[ref]

The approximately 66 Ma skeleton of Adalatherium expanded that evidence into the postcranial skeleton. It documents a relatively large, several-kilogram non-therian mammal with an unusual combination of cranial, dental, vertebral and limb features. This contradicts the caricature that all Mesozoic mammaliaforms were anatomically interchangeable tiny insect-eaters. Madagascar's long isolation provides a plausible context for its evolutionary distinctiveness, but the claim that isolation caused a particular feature remains an explanatory hypothesis. One needs comparative island and continental samples to distinguish an island effect from inherited lineage-specific anatomy. ^[ref]

Australia's early Eocene Djarthia, approximately 55 Ma, addresses a different issue: the relationships and movement of marsupials. Its ankle material supports a position close to the base of Australidelphia, a group containing the living Australian orders and the South American Microbiotheria. This is stronger evidence than assuming that every small Australian jaw belongs inside a modern Australian family. ^[ref] It is compatible with a history involving South America and Antarctica, but a branching order is not a map of a single migration. An extinct distribution can be extensive, intermediate populations can disappear, and the oldest sampled fossil need not occur near the place where a lineage originated. Also, the older and more inclusive Metatheria must not be confused with the living marsupial crown group.

Together these discoveries change how large-scale history is tested. First, expanding southern sampling can overturn a supposed absence that arose from collecting intensity, exposure of suitable rocks or preservation. taphonomy and the concentration of many early records on durable teeth must be modelled before comparing continental diversity. Second, new skeletons can change the inferred phylogenetic tree, and therefore whether a tooth adaptation counts as one origin or several. Third, fossil calibration constrains the minimum age of a lineage, with explicit uncertainty in both geological age and phylogenetic assignment. Fourth, continental drift changes which dispersal routes were physically plausible. Shared distributions across former Gondwana may reflect vicariance, later dispersal, or a mixture; the geological separation must be compared with a defensible lineage age rather than used as its automatic explanation.

From the Jurassic through the Palaeogene, these independent discoveries have cumulatively changed both the anatomical evidence and its interpretation. They reveal a more diverse southern mammaliaform history and force explicit tests of convergence, missing data and geographic sampling, rather than replacing an assumed northern centre with an equally assumed southern centre.

An Early Jurassic frog relative with a derived caudopelvic apparatus interpreted as consistent with jumping.