By looking at the chemistry of rocks deposited during that time period, specifically coupled carbon and sulfur isotope data, a research team led by University of California, Riverside biogeochemists reports that oxygen - free and hydrogen sulfide -
rich waters extended across roughly five percent of the global ocean during this major climatic perturbation — far more than the modern ocean's 0.1 percent but much less than previous estimates for this event.
Not exact matches
Shelf
waters off the Pacific Northwest
extend anywhere from 30 to 80 kilometers offshore and lie beneath the California Current, one of the
richest marine ecosystems in the world.
Hydrothermal vents form by an analogous method: Ion -
rich hot
water is expelled from the seafloor and then begins to dissolve, forming a porous shell of metal
extending upward.
Langebaan Lagoon
extends in a finger of
water away from Saldanha Bay, its 16 kilometres controlled by tidal currents, tailing off into salt marshes and a cluster of salt pans,
rich with
water bird life.