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Plate tectonics changes the environments in which natural selection, gene flow and extinction operate. It influences both the persistence of habitable conditions and the geographical and chemical opportunities for evolution. It does not prescribe a unique sequence of biological innovations.

Separation of continents by continental rifting divides populations and reduces gene flow, promoting allopatric speciation. Continental collision or newly exposed land connections can reunite populations, permit dispersal and introduce competitors or predators. These mechanisms connect biogeography to continental configuration. Changing the amount and fragmentation of shallow continental shelf habitat can also change the opportunities for diversification of marine organisms.

Over long intervals, volcanic outgassing, silicate weathering, carbonate burial and subduction exchange carbon among the interior, atmosphere and ocean. In a suitable regime, warmer, wetter conditions increase silicate weathering, remove atmospheric carbon dioxide and weaken the greenhouse effect. This negative feedback can support long-lived habitability, though it depends on exposed fresh rock, available water and reaction rates.^[ref] Mountain building changes precipitation, erosion and delivery of nutrients to the ocean, affecting primary production and organic carbon burial.

The opening and closure of ocean gateways changes ocean circulation, transport of heat and the supply of oxygen to deep water. Together with movement of land through different latitudes and changes in sea level, this reorganizes climate and habitat. Enhanced organic carbon burial can change atmospheric oxygen over long intervals, while a poorly ventilated ocean can develop ocean anoxia. Such chemical changes alter which forms of metabolism are viable.

Hydrothermal circulation at spreading ridges and through fractured rock supplies chemical disequilibrium and mineral surfaces. For example, serpentinization can produce hydrogen usable by chemolithotrophy when suitable electron acceptors are available. This supplies a possible setting for abiogenesis and early ecosystems; it does not establish that life originated there.

There can also be abrupt disruption. Rapid emplacement of a large igneous province can change climate through gas release; sulfur-bearing aerosols can initially cool, whereas sustained carbon dioxide release can warm and contribute to ocean acidification and ocean anoxia. Such perturbations can contribute to mass extinction, followed by adaptive radiation among survivors. The Deccan Traps exemplify the scale of volcanism involved, but their association with the Cretaceous–Palaeogene boundary does not justify attributing the entire biological crisis to volcanism alone. Both gradual environmental reorganization and rare rapid perturbations belong in the explanation.

There is no general basis for assigning behaviour a smaller causal role in macroevolution. Its immediate effects are usually easier to measure within populations, but those effects can alter lineage formation and persistence. The comparison needs a definition of “contribution”: the proportion of evolutionary changes initiated by behaviour, their magnitude, their necessity, or the strength of available evidence would give different answers. Microevolution concerns change within biological populations; macroevolution concerns patterns at and above the level of species, including speciation, adaptive radiation and extinction. They are connected processes with different objects of measurement.

At the population scale, animal behaviour changes who encounters which resources, survives, mates and reproduces. Habitat preference changes exposure to ecological natural selection; mate choice changes reproductive success; dispersal changes the spatial distribution of alleles. Behaviour can therefore affect the evolution of other traits even if the behaviour itself does not evolve. Conversely, an environmentally induced change in behaviour is not automatically evolutionary change. Learning and phenotypic plasticity can occur within one lifetime, whereas an evolutionary claim requires persistence through inherited differences or an explicitly specified process of cultural inheritance.

A simple population genetics calculation makes the distinction concrete. Let $x_i$ be an individual's number of copies of a focal allele, $w_i$ its contribution to reproduction, and $p=\mathbb{E}(x)/2$. With unbiased Mendelian segregation and no other transmission change, the expected allele frequency after selection satisfies:Behaviour can change $w$ and thereby change the covariance, whether selection acts directly on a behavioural difference or on another trait whose consequences depend on behaviour. The equation does not imply that every correlation between a behaviour and reproductive success is genetic: common environment, age and condition can generate such correlations. A common garden experiment, a pedigree and measurements across environments help identify the inherited component.

Behaviour may expose a previously uncommon phenotype to selection. Foraging in a new habitat can make a different resource profitable, after which selection can refine feeding structures or behavioural response thresholds. Laboratory competitions between spadefoot tadpoles from populations differing in expression of a carnivore ecomorph found differences in resource capture and morphology consistent with adaptive refinement of a formerly plastic response. Expression without the inducing cue also supported genetic assimilation. ^[ref] This is a combination of behaviour and development, not proof that behaviour universally comes first. Genetic accommodation requires evolution of the response, rather than assuming that an acquired habit is copied directly into DNA.

The opposite effect is also possible. Through phenotypic buffering, movement or flexible foraging may keep individuals in suitable conditions and reduce selection on physiological or morphological differences. Thus flexibility can promote occupation of a new environment, delay genetic divergence, or prevent local extinction. The sign depends on whether behaviour changes exposure to selection or allows animals to avoid it. A short-term adaptive response is consequently not evidence for a universal acceleration of evolutionary change.

At the boundary between populations and species, the behavioural effects are particularly direct. Assortative mating, host choice and learned signals can reduce gene flow. In the Big Bird lineage of Darwin's finches, field observations and genomic ancestry documented an immigrant Geospiza conirostris breeding with a resident Geospiza fortis and the formation of an endogamous descendant lineage. Song and distinctive morphology contributed to mating within that lineage. ^[ref] The evidence links immigration, hybridization and mate recognition to rapid reproductive separation; it does not show that song alone caused isolation or establish the lineage's indefinite future persistence. Nevertheless, behaviour participates in an event conventionally classified as macroevolution.

Over longer periods, these mechanisms can influence the rates of lineage origination and disappearance. Behaviour that permits colonization can expose populations to ecological opportunity and eventual adaptive radiation. Specialization in host use or mating signals can strengthen reproductive barriers. Conversely, costly reproductive competition or inflexible resource use can increase vulnerability. In fossil ostracods, greater sexual dimorphism was associated with greater estimated extinction risk, using carapace differences as a proxy for male reproductive investment. ^[ref] This is unusually direct evidence about actual lineage loss, but an anatomical proxy does not preserve courtship or experimentally isolate sexual selection from every correlated attribute. It supports a possible connection rather than a general law that strong sexual selection causes extinction.

Evaluating a claim about relative importance also requires correcting unequal evidence. Contemporary behavioural experiments can manipulate cues and follow reproduction, whereas most ancient behaviour must be inferred from traces, anatomy or living relatives. Living-only comparative studies omit extinct lineages and can confuse a trait associated with diversification with a trait that evolved after diversification. Comparisons should allow for shared ancestry, environmental opportunity and incomplete sampling, and distinguish an increased speciation rate from a reduced extinction rate. Counting observed behavioural changes over years against anatomical changes over millions of years is not a meaningful common denominator.

Behaviour has demonstrable population-level effects and plausible, sometimes well-documented effects on speciation and extinction. The stronger conclusion is that its evolutionary influence is context-dependent and transmitted across scales, while the evidence becomes harder to identify over deep time. A qualified statement about evidential accessibility is defensible; a general ranking of causal importance is not.