Question

Passage:
In the late eighteenth and early nineteenth centuries, the burgeoning field of geology was characterized by a profound debate regarding the mechanisms and timeframe of the Earth’s formation. Prior to this period, the dominant paradigm was heavily influenced by literal interpretations of scriptural chronology, which posited an Earth no more than a few thousand years old. The first significant departure from this framework was articulated by the Scottish natural philosopher James Hutton in his 1788 work *Theory of the Earth*. Hutton introduced the concept of "deep time," arguing that the geological features of the Earth could not be explained by brief, violent events, but rather were the result of slow, continuous processes—such as erosion and sedimentation—operating over unimaginably long periods. Crucially, Hutton theorized that subterranean heat was the primary engine driving the cyclical uplift of new landmasses, a mechanism he deemed necessary to prevent the Earth's surface from eventually eroding entirely beneath the oceans.

Conversely, the French naturalist Georges Cuvier, observing distinct breaks in the fossil record within the Paris Basin, championed the theory of catastrophism. Cuvier meticulously documented sudden disappearances of various faunal assemblages across distinct geological strata. He concluded that the Earth’s history was punctuated by localized, sudden, and violent upheavals—such as massive floods—that drove regional populations to extinction. Notably, Cuvier did not attribute these catastrophes to divine intervention, nor did he initially insist they were global in scale, but rather viewed them as empirical realities mandated by the discontinuity of the fossil evidence.

Building upon Hutton’s foundation, the British geologist Charles Lyell synthesized and popularized the uniformitarian framework in his seminal *Principles of Geology* (1830–1833). Lyell advanced a strict methodological principle: the forces that shaped the Earth's surface in the past are exactly the same in kind and intensity as those observable in the present. Unlike Hutton, who relied heavily on the theoretical necessity of subterranean heat, Lyell grounded his arguments in exhaustive empirical observations of contemporary phenomena, such as the gradual building of river deltas and the slow action of modern volcanoes. Furthermore, Lyell extended uniformitarianism to the biological realm, arguing that the fossil record’s apparent abrupt transitions were merely artifacts of an incomplete geological archive, rather than evidence of Cuvier's catastrophes.

While Lyell's strict uniformitarianism became the guiding paradigm for nineteenth-century geology, modern geologists have come to recognize that both gradual processes and sudden catastrophic events—such as asteroid impacts or massive volcanic eruptions—have played roles in shaping the planet. Nevertheless, the explicit factual claims established by these early pioneers formed the crucible of modern earth science. Hutton's introduction of deep time broke the constraints of historical chronology; Cuvier's insistence on the reality of extinction established paleontology as a rigorous discipline; and Lyell's methodological constraint ensured that geological theories were anchored in observable mechanisms.

Question:
Based strictly on the explicit information provided in the passage, match each of the following scientific figures with the specific geological or methodological claim attributed to them in the text.