How worms influenced evolution by increasing atmospheric oxygen

Amazing stuff!

"... The digging of prehistoric worms and other invertebrates churned up sediment along the ocean floor, exposing some minerals and burying others beneath layers of mud, silt, and sand. When scientists examined mixed sediments in the Chesapeake Bay, where conditions closely mimic those found in the early ocean, they found surprisingly high levels of pyrite—a mineral that releases oxygen when it forms but dissolves when exposed to oxygen in the water. Burrowing worms would have helped bury newly-formed pyrite while also unearthing the chemicals needed to make more of it, thereby releasing more oxygen and allowing it to build up rapidly in the atmosphere. ...
This steep increase in atmospheric oxygen kickstarted what is known as the Great Ordovician Biodiversification Event, which occurred about 480 million years ago and spawned a spectacular diversity of new animal species ..."

From the abstract:

"The early Paleozoic Era (∼540–420 Ma) was an interval of profound biogeochemical changes including increasing oxygen (O2) and the onset of bioturbation (sediment mixing by animals). It is hypothesized that incipient bioturbation caused a monotonic decrease in sedimentary burial of pyrite (FeS2), which would have slowed atmospheric O2 accumulation. However, pyrite accumulation can exhibit complex responses to dynamic, low-O2 environmental conditions. To assess pyrite burial in a potential modern analogue to early Paleozoic environments, we collected sediment cores from the Chesapeake Bay, an estuary with multiple gradients in sulfate concentration, hypoxia intensity, organic carbon flux and lability, and bioturbation. Results indicate that pyrite accumulation is maximized not under strong sulfate depletion in highly reducing sediments, but rather in sediments that occupy the mid-range of sulfate–chloride ratios. This probably occurs through efficient replenishment of pore water sulfate and/or through the generation of sulfur redox intermediates, which promote pyrite formation via the polysulfide reaction pathway. In light of these results and in contrast to earlier models, we hypothesize that mild early Paleozoic bioturbation temporarily increased pyrite burial efficiency by stimulating higher sulfate reduction rates and increasing sedimentary sulfide retention. Compiled sulfur and carbon data from a geochemical database indicate that median sulfur-carbon ratios of fine-grained marine siliciclastic rocks increased from the Ediacaran through the Ordovician, then decreased and became much less variable from the Silurian onward. Thus, the Cambrian and Ordovician Periods may constitute a distinct interval of the Proterozoic-Phanerozoic transition in which bioturbation temporarily accelerated O2 buildup. This transition probably ended in the Silurian, when pO2 rose to sufficient levels to homogenize sedimentary carbon–sulfur cycling."

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Trends in estuarine pyrite formation point to an alternative model for Paleozoic pyrite burial (open access)