There was a warm, stable climate with dispersed continents surounded by vast warm and
shallow seas over continental shelves that provided light, oxygen, and nutrients for life to thrive in, because intense mountain - building also increased erosion and the discharge of eroded nutrients into those seas.
Not exact matches
Place them into a
shallow, foil - lined baking tray then splash
over some good olive oil, some aged balsamic, red wine vinegar, water,
sea salt and cracked pepper (I don't strictly follow any quantities here... basically, you want to create enough liquid for the beetroot to initially steam, then caramelise with a sticky, delicious glaze.
You could call it that, all right, when you saw how the tides clashed with the wind
over the
shallow reefs round Blasket, and the long - toothed rocks came clear out with the
sea running back off them, and the black sleek heads of the brave seals bobbing in the swells.
Plankton, crustaceans and fish, all food for wildlife, reproduce at the dynamic edge of the
sea ice, where it floats
over shallow near - shore waters.
The Russian and American scientists have never before experienced anything of such magnitude, and in addition to powerful emissions from
shallow waters where
over 100 readings were recorded, it is spewing up from within cracks in the Arctic ice in the open
seas far from land.
Basically, although the gas is indeed easily absorbed by
sea - water, it is the timescales that matter: mixing of
shallow and deep oceanic waters takes place
over hundreds to thousands of years but
sea - water can de-gas parts of its carbon dioxide payload
over much, much shorter periods.
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.
It's as blurry and fluid as the slope of the shore, from beach to the
shallows to water
over your head to the open
sea.
Ambergris is 25 miles long and a little
over a mile wide, in some places, and it is located in the clear
shallow waters of the Caribbean
Sea just off the tip of Mexico's Yucatan Peninsula.
Named for its characteristic reef development, this dive site features a profile with two distinct reef zones
over a distance of about 800 ft.. A
shallow reef extends from
sea level to 40 ft and a deeper reef begins at 70 ft, extending to more than 100 ft at the wall.
1.15 - Flying out to
sea over the coast line,
over shallow, murky water, dominated by mud and very fine sand brought to the
sea from the Belize River.
The eastern North Pacific stock of gray whales prefers
shallow, coastal waters and feeds
over oceanic continental shelves around the northern Bering and southern Chukchi
seas between Alaska and Russia during the summer.
In the
shallow areas be sure to keep your eyes open for peacock flounders, octopus, needlefish and turtles or drop down a little deeper
over dense coral growth to see puffers, moray eels, parrot fish, lobsters, and even
sea horses.
Under the
sea off the shores of Punta Cancún, Manchones Reef, and Punta Nizuc lie
over 400 humanoid statues,
shallow enough for snorkelers, divers, and glass - bottom boats to see.
Soak up stunning views of the lush coast and turquoise
sea as you cruise
over to a
shallow lagoon for a stingray experience.
This flight gives the most unique views by flying at a low altitude
over the
shallow flats of the Keys, and visitors get the chance to see marine wildlife such as
sea turtles, dolphins and sharks from above.
Initially,
shallow circulations driven by differential radiative cooling induce a self - aggregation of the convection into a single band, as has become familiar from simulations
over idealized
sea surfaces.
At the risk of oversimplifying, the effects of groundwater storage can be differentiated between
shallow - aquifer effects that modulate global
sea level on year to year and decade to decade timeframes, versus deep aquifer effects that modulate
sea level trends
over centuries and millennia.
coral cover was positively correlated with the mean
sea level experienced
over the preceeding months... the overall picture for these
shallow reefs is a positive one as they respond to increasing
sea level and show rapid recovery from environmental disturbances.
Elevated pb signals are observed
over deep extratropical regions (e.g., Southern Ocean basins) and
shallow or semi-enclosed areas (e.g., Indonesian and Nordic
seas).
Thus, to whelp in April and still remain for
over shallow feeding grounds, seals are coincidentally surrounded by extensive winter
sea ice.
As it happens, the extra heat travels into
shallow seas along the continental shelf and,
over time, the warming also spreads to the deep seabed, destabilizing methane hydrates and free gas trapped
over millennia in the permafrost cap.
Seventy - five percent (75 %) of the
sea over the shelf is
shallow water, less than 50 metres deep, and consequently more immediately exposed to warming trends.
Over time, building subsea pipeline networks could become an export area for Australia in building similar networks in Asia, specifically the
shallow South China
Sea.
http://earthobservatory.nasa.gov/IOTD/view.php?id=83672 http://www.nytimes.com/2014/05/13/science/earth/collapse-of-parts-of-west-antarctica-ice-sheet-has-begun-scientists-say.html It will add about 10 feet according to an interview with one of the scientists involved; but
over a long time and fairly vague time frame, unless reinforcing processes (carbon release from melting permafrost,
shallow ocean bottom warmingn in the form of methane from clathrates), a major reduction in earth's albedo from permafrost, net ice sheet, and total
sea ice, continue to increasingly accelerate the process.
The University of Western Australia's Ryan Lowe led a team of researchers who studied a reef system off the coast of northwestern Australia, as well as other reef systems across the globe, in order to develop a new model for predicting how rapid
sea level rise will impact daily water temperature extremes within these
shallow reefs
over the next century.
However, studying
shallow waters does not form an accurate representation of the interactions that happen
over the deep
sea.
What are telling observations against the hypothesis of a largely internally driven imbalance are, on the one hand, the fact the
sea level variations are relentlessly positive, irrespective the phase of the PDO, and, on the second hand, the fact that the rate of warming
over land is larger than it is
over sea (and also that the
shallow (0 - 700m) ocean layer never actually cools).
Basically, although the gas is indeed easily absorbed by
sea - water, it is the timescales that matter: mixing of
shallow and deep oceanic waters takes place
over hundreds to thousands of years but
sea - water can de-gas parts of its carbon dioxide payload
over much, much shorter periods.