Cretaceous Terrestrial Revolution

The Cretaceous Terrestrial Revolution (abbreviated KTR), also known as the Angiosperm Terrestrial Revolution (ATR) by authors who consider it to have lasted into the Palaeogene, describes the intense floral diversification of flowering plants (angiosperms) and the coevolution of pollinating insects, as well as the subsequent faunal radiation of frugivorous, nectarivorous and insectivorous avians, mammals, lissamphibians, squamate reptiles and web-spinning spiders during the Middle to Late Cretaceous, from around 125 Mya to 80 Mya. Alternatively, according to Michael Benton, the ATR is proposed to have lasted from 100 Ma, when the first highly diverse angiosperm leaf floras are known, to 50 Ma, during the Early Eocene Climatic Optimum, by which point most crown lineages of angiosperms had evolved.

Appearance of angiosperms
Molecular clock analyses of angiosperm evolution suggest that crown group angiosperms may have diverged up to 100 million years before the start of the KTR, although this is possibly due to artefacts of the inabilities of molecular clock estimates to account for explosive accelerations in evolution that may have caused the extremely fast diversification of angiosperms shortly after their first appearance in the fossil record.

Causes
The KTR was enabled by the dispersed positions of the continents and the formation of new oceans during the Cretaceous in the aftermath of Pangaea's breakup in the preceding Jurassic period, which enhanced the hydrological cycle and promoted the expansion of temperate climatic zones, fuelling radiations of angiosperms.

Another cause of the explosive angiosperm diversification was the evolution of leaf vein densities greater than 2.5–5 mm/mm2, when the leaf interior transport path length of water became shorter than the leaf interior transport path length of CO2. This enabled greater utilisation of CO2 and gave an evolutionary advantage to flowering plants over conifers because they could sequester more CO2 for the same amount of water. The much greater capacity of angiosperms for assimilating CO2 sharply increased global bioproductivity.

Angiosperms enabled more frequent fires than gymnosperms, and they also recovered more quickly from fires than gymnosperms did. This created a feedback loop that advantaged angiosperms over gymnosperms during the Cretaceous.

Biotic effects
Although angiosperm diversity drastically grew over the Cretaceous, this did not necessarily translate to ecological dominance, which they only achieved in the Early Cenozoic.

Angiosperms responded to increasing coevolution with frugivores by enlarging the sizes of their fruits, which peaked during the Early Eocene.

Before Lloyd et al.'s 2008 paper described the KTR, it had been widely accepted in paleontology that new families of dinosaurs evolved during the Middle to Late Cretaceous, including the euhadrosaurs, neoceratopsians, ankylosaurids, pachycephalosaurs, carcharodontosaurines, troodontids, dromaeosaurs and ornithomimosaurs. However, the authors of the paper have suggested that the apparent "new diversification" of dinosaurs during this time is due to sampling biases in the fossil record, and better preserved fossils in Cretaceous age sediments than in earlier Triassic or Jurassic sediments. However, later studies still suggest the possibility that the KTR caused a rise in dinosaur diversity. Dinosaurs contributed little to angiosperm diversification, which was instead mainly driven by coevolution with other animals, such as insects and herbivorous mammals. It has been suggested that some pterosaurs may have been seed dispersers symbiotically linked to angiosperms. A comprehensive molecular study of evolution of mammals at the taxonomic level of family also showed important diversification during the KTR. Mammals have been found to have decreased in disparity during the KTR.

Insect diversity overall appears to have been minimally affected by the KTR, as molecular evidence shows that the increase in diversity of pollinating insects was asynchronous with the KTR. However, Early Cretaceous angiosperms were short in stature and would have been heavily reliant on insect pollination, and fossil remains of early angiosperms suggest such a dependence on zoophilous pollination. Genetic evidence indicates a major radiation of phasmatodeans occurred during the KTR, likely in response to a coeval radiation of enantiornitheans and other visual predators. Ants likewise underwent massive increase in diversity as part of the KTR. Similarly, bee pollinator diversification strongly correlates with angiosperm flower appearance and specialization during the same era. Flies, already successful pollinators before the rise of angiosperms, quickly adapted to the new hosts. Beetles became pollinators of angiosperms by the earliest part of the Late Cretaceous. Lepidopterans radiated during the KTR, though the angiosperm radiation is insufficient in and of itself to completely account for their diversification. Among one lineage of sawflies, there was a change in preferred host plants amidst the biotic reorganisation of the KTR. Not all insects were advantaged by this diversification and rearrangement of ecosystems; long-proboscid insects that were mainstays of gymnosperm-dominated ecosystems earlier in the Mesozoic underwent a major decline. Late-surviving eoblattodeans evolved long, slim bodies with long external ovipositors in response to the angiosperm radiation, but this proved to be an evolutionary dead end in the long run and the group went extinct. The so-called "golden age" of neuropterans during the Middle Mesozoic, when gymnosperms dominated the flora, ended with the KTR and its reshaping of the terrestrial environment.

The KTR may have supercharged the contemporary Mesozoic Marine Revolution (MMR) by enhancing weathering and erosion, accelerating the flow of limiting nutrients into the world’s oceans.

For nearly the entirety of Earth's history, including most of the Phanerozoic eon, marine species diversity exceeded terrestrial species diversity, a pattern which was reversed during the Middle Cretaceous as a result of the KTR in what has been termed a biological "great divergence", named after the historical Great Divergence.