Paleoclimatologists investigating the Cretaceous oceanic anoxic events (OAEs) have established a definitive causal sequence initiated by massive submarine volcanism. The formation of Large Igneous Provinces released vast quantities of carbon dioxide into the atmosphere. This sudden spike in greenhouse gases precipitated a period of intense, rapid global warming. Consequently, the elevated global temperatures accelerated the hydrological cycle, leading to a marked increase in the chemical weathering of continental silicate rocks. This accelerated weathering washed massive influxes of terrestrial nutrients, primarily phosphorus, into the ocean basins. The resulting nutrient surplus triggered unprecedented phytoplankton blooms in the photic zone. As these massive algal populations inevitably died and sank, their subsequent decomposition by aerobic bacteria in the water column consumed staggering amounts of dissolved oxygen. Ultimately, this severe oxygen depletion resulted in the widespread anoxic conditions that characterize the sediment record of these periods.
Based exclusively on the detailed mechanism described above, arrange the following phenomena in the chronological causal order of their occurrence, from the earliest catalyst to the final consequence:
- 1A significant increase in atmospheric greenhouse gas concentrations
- 2Enhanced chemical degradation of terrestrial silicate rocks
- 3A surge in oceanic phosphorus and other nutrient levels
- 4Unprecedented growth of photosynthetic marine organisms
- 5Extensive consumption of dissolved oxygen during biological decay