Modern reef-building corals only thrive within a narrow sea surface temperature range of about 22–30°C. The authors use this preference as an independent check on past climate models, running an ensemble of simulations from 250 million years ago to today across a range of CO2 levels and paleogeographies. Their coral-constrained temperature curve closely matches earlier … Read more…
The mid-Proterozoic interval between 1800 and 800 Ma, commonly referred to as the “Boring Billion”, was marked by the emergence of eukaryotic cells from prokaryotic ancestors, a key step in the evolution of life. This period encompassed the assembly and dispersal of two consecutive supercontinents, Nuna and Rodinia, as well as the development of extensive … Read more…
The long-term diversification of the biosphere responds to changes in the physical environment. Yet, over the continents, the nearly monotonic expansion of life started later in the early part of the Phanerozoic eon1 than the expansion in the marine realm, where instead the number of genera waxed and waned over time2. A comprehensive evaluation of … Read more…