Enormous amounts of freshwater were released into the North Atlantic following deglaciation, and an influx of freshwater into the North Atlantic
Deep Water formation zone can potentially trigger abrupt climate changes.
Not exact matches
This research not only provides the first clear evidence that microorganisms were directly involved in the deposition of Earth's oldest iron
formations; it also indicates that large populations of oxygen - producing cyanobacteria were at work in the shallow areas of the ancient oceans, while
deeper water still reached by the light (the photic
zone) tended to be populated by anoxyenic or micro-aerophilic iron - oxidizing bacteria which formed the iron deposits.
It seems significant that it is happening simultaneously in both the southern and northern hemispheres, suggesting freshening in
deep / bottom
water formation zones, which would be slow enough to dampen seasonal effects.