The correct order for ecological succession in reefs is as follows: pioneer comm
ID: 292197 • Letter: T
Question
The correct order for ecological succession in reefs is as follows:
pioneer community as moundlike and broad corals, intermediate stage with sticklike corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as sticklike corals, intermediate stage with moundlike and broad corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as rogusan and tabulate corals, intermediate stage with moundlike and broad stromatoporids, and mature stage with the reef near to sea level with tabulate coral- and bryozoan-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as sticklike corals, intermediate stage with moundlike and broad corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by moundlike and broad corals
What evidence is there that climatic cooling caused the Late Devonian mass extinction?
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, decline of limestone production, and extinction of cool-water marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, increase of limestone production, and extinction of tropical marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward lighter values, decline of limestone production, and extinction of tropical marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, decline of limestone production, and extinction of tropical marine species.
pioneer community as moundlike and broad corals, intermediate stage with sticklike corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as sticklike corals, intermediate stage with moundlike and broad corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as rogusan and tabulate corals, intermediate stage with moundlike and broad stromatoporids, and mature stage with the reef near to sea level with tabulate coral- and bryozoan-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
pioneer community as sticklike corals, intermediate stage with moundlike and broad corals, and mature stage with the reef near to sea level with stromatoporoid-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by moundlike and broad corals
What evidence is there that climatic cooling caused the Late Devonian mass extinction?
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, decline of limestone production, and extinction of cool-water marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, increase of limestone production, and extinction of tropical marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward lighter values, decline of limestone production, and extinction of tropical marine species.
The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, decline of limestone production, and extinction of tropical marine species.
Explanation / Answer
C, pioneer community as rogusan and tabulate corals, intermediate stage with moundlike and broad stromatoporids, and mature stage with the reef near to sea level with tabulate coral- and bryozoan-encrusted ridges on the outside and a quiet lagoon in the middle inhabited by twiglike fragile corals
B. The spread of glaciers in Gondwanaland, shifts of oxygen isotopes in conodonts toward heavier values, increase of limestone production, and extinction of tropical marine species.
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