They are pinnacle reefs, built by cyanobacteria on
the shallow sea floor 543 million years ago, during a time known as the Ediacaran period.
Not exact matches
In a
shallow part of the
sea floor underneath the ice shelf, a bedrock protrusion, named the Bawden Ice Rise, has served as an anchor point for the floating shelf for many decades.
But with climate change, the WAP is experiencing rapid regional warming, with fewer days each year of fast ice — letting the icebergs into the
shallows more often, where they carve huge gashes through the habitat of the colorful, tentacled invertebrate animals carpeting the
sea floor.
During this time, large (up to meter - sized) soft - bodied organisms, often shaped like discs or fronds, had lived on or in
shallow horizontal burrows beneath thick mats of bacteria which, unlike today, coated the
sea floor.
That leads them to suggest that the concentration of lumps may have come about when a large number of whales died and then sank to the
sea floor, where the carcasses quickly decomposed in the warm,
shallow waters but the ambergris — which on its own typically floats — was buried and preserved.
In a separate finding published this week, another research team reports teasing out plankton DNA that's up to 11,400 years old from the
floor of the much
shallower Black
Sea.
For two hundred years, fleets of treasure galleons stuffed with silver and gold and emeralds had plied the Caribbean
Sea, crisscrossed it every which way, from Key West down to Cartagena, from the Yucatán over to the Windward Islands, and every so often, one of those unpredictable West Indian cyclones would come spinning across the Caribbean and slam half the fleet onto
shallow reefs, which ripped open the hulls and spewed that treasure all over the ocean
floor.
Like the modern Gulf of Mexico, this
shallow Cretaceous
sea was occasionally subject to violent storms that disturbed the
floor of the
sea.
Most of the members of the clam family are bottom dwellers, usually
shallow water, and with some exceptions, move slowly across or under the
sea floor surface while a few are fixed in one place.
The fringing reefs here are
shallow and slope gently to the
sea floor.
This is a very
shallow reef network with a sandy
sea floor at around 14m with the reef rising to a couple of metres below the surface.
The scariest parts of the Siberian margin are the
shallow parts, because this is where methane bubbles from the
sea floor might reach the surface, and this is where the warming trend is observed most strongly.
For quite interesting reasons, the
sea -
floor in
shallow waters north of Siberia is frozen.
Now come fears of a methane time bomb, part two, this one bursting from the
sea floor of the
shallow Arctic continental shelf.
Much of the color likely comes from resuspended sediment dredged up from the
sea floor in
shallow waters.