The formation process of coral reef zonation was summarized by drilling results and trench observations in several fringing reefs in the central Ryukyu Islands. The prototype of reef zonation emerged when the reef first reached sea level as an offshore barrier in the middle Holocene. Then, reef has expanded seaward by development of reef edge spurs under the almost stable sea level condition in the late Holocene. Contrary to the reef which first reached sea level at offshore, obscure zonal pattern is formed where the initial growth axis lies at the landward end because of no energy related gradient during reef development
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.In co...
ABSTRACT. Published geological studies of the Capricorn and Bunker Groups of reefs together with pre...
Many factors govern reef growth through time, but their relative contributions are commonly poorly k...
Within the lndo-Pacific region Holocene reef development over tlie last 6000 yBP has occurred during...
Modern fringing reefs of Yoron Island, Ryukyu Arc, Japan, have been investigated for the purpose of ...
Holocene emerged coral reefs develop at the Gushichan coast in the southern Okinawa Island, the Ryuk...
Ryukyu Islands are an active island arc on the island shelf in high latitude between the Ryukyu Tren...
This thesis defines the response in two time frames, of individual reefs and coral reef ecosystems t...
Well-developed Holocene raised coral reef terraces are formed in Kodakara Island (29°13'N 129°19'E),...
Fringing reefs are generally not simple veneers of coral growth along tropical shorelines. Extensive...
Four drilling cores are observed from a high-latitude coral reef at the northwestern Mage Island (N3...
The stratigraphy of fringing coral reef environments and platforms provides unique insights into ree...
The geomorphology and chronostratigraphy of the reef flat (including microatoll ages and elevations)...
The universally known subsidence theory of Darwin, based on Bora Bora as a model, was developed with...
The fossil record provides valuable data for improving our understanding of both past and future ree...
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.In co...
ABSTRACT. Published geological studies of the Capricorn and Bunker Groups of reefs together with pre...
Many factors govern reef growth through time, but their relative contributions are commonly poorly k...
Within the lndo-Pacific region Holocene reef development over tlie last 6000 yBP has occurred during...
Modern fringing reefs of Yoron Island, Ryukyu Arc, Japan, have been investigated for the purpose of ...
Holocene emerged coral reefs develop at the Gushichan coast in the southern Okinawa Island, the Ryuk...
Ryukyu Islands are an active island arc on the island shelf in high latitude between the Ryukyu Tren...
This thesis defines the response in two time frames, of individual reefs and coral reef ecosystems t...
Well-developed Holocene raised coral reef terraces are formed in Kodakara Island (29°13'N 129°19'E),...
Fringing reefs are generally not simple veneers of coral growth along tropical shorelines. Extensive...
Four drilling cores are observed from a high-latitude coral reef at the northwestern Mage Island (N3...
The stratigraphy of fringing coral reef environments and platforms provides unique insights into ree...
The geomorphology and chronostratigraphy of the reef flat (including microatoll ages and elevations)...
The universally known subsidence theory of Darwin, based on Bora Bora as a model, was developed with...
The fossil record provides valuable data for improving our understanding of both past and future ree...
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.In co...
ABSTRACT. Published geological studies of the Capricorn and Bunker Groups of reefs together with pre...
Many factors govern reef growth through time, but their relative contributions are commonly poorly k...