造礁珊瑚

高雄上更新统造礁珊瑚及其地质学上之意义

Upper Pleistocene reef corals from Kaohsiung ( takao ) and their geological significance

热带海洋环境研究的新代用指标&造礁珊瑚~（14）C记录

A new proxy of tropical ocean environmental study : radiocarbon record of hermatypic coral

造礁珊瑚骨骼δ~（13）C及其反映的环境信息研究概况

General Situation of the Study on Reef Coral δ ~ ( 13 ) C and the Related Environment information

造礁珊瑚δ~（18）O记录的过去气候研究进展

Developments in the Study of Reef Coral δ ~ ( 18 ) O Recorded Past-Climate

在这次评估中，他们也列入了对小龙虾、淡水蟹类、造礁珊瑚和头足类动物的综合评价。

They also included comprehensive assessments ofcrayfish , freshwater crabs , reef-building corals and cephalopods in theevaluation .

我因此得以研究太平洋中的小岛所构成的造礁珊瑚体系。

So I was able to study the madreporic process that has created the islands in this ocean .

大块的造礁珊瑚，有盘旋的和沟回的表面。中二叠世&新近纪新特提斯洋构造域旋回。

Massive reef-building coral having a convoluted and furrowed surface . ( 3 ) MiddlePermian-Neogene extension-compression cycle of Neo-Tethys .

这些悬崖大半是称为千孔珊瑚、滨珊瑚、星珊瑚和脑形珊瑚的造礁珊瑚类的杰作。

These walls were the express achievements of madrepores known by the names fire coral , finger coral , star coral , and stony coral .

土地差不多完全是由造礁珊瑚沉积形成的，但有些干涸了的急流河床，间杂有花岗石的残余，说明这岛的形成是在原始的太古时期。

The soil was almost entirely madreporic , but certain dry stream beds were strewn with granite rubble , proving that this island was of primordial origin .

造礁珊瑚是研究热带海洋环境变化的极好材料，珊瑚骨骼δ~（18）O分析是提示其所记录的环境信息的重要手段。

Reef coral has proved to be an excellent material with which to research into the tropical ocean environment , and its skeleton δ 18O is an important tracer for analyzing the recorded environmental information .

造礁珊瑚跟普通珊瑚不能混为一谈，它们的纤维组织蒙上一层石灰质的表皮，表皮构造的各种变化使我著名的老师密尔？爱德华先生把它们分为五部。

Madrepores , which one must guard against confusing with precious coral , clothe their tissue in a limestone crust , and their variations in structure have led my famous mentor Professor Milne-Edwards to classify them into five divisions .

造礁珊瑚类动物在海波激荡的表面一层特别繁衍，因此，它们的造礁工作是从上层开始，渐次及于下层的，上层带着剩余的分泌物，渐渐沉到下面去。

These polyps grow exclusively in the agitated strata at the surface of the sea , and so it 's in the upper reaches that they begin these substructures , which sink little by little together with the secreted rubble binding them .

达尔文的学说就是这样，他应用这学说来说明环状珊瑚岛的构成——照我的意思，这学说比那以海面下几米有浮出的山岭或火山的峰顶作为造礁珊瑚的工作基地的学说，较为优越，较为合理。

This , at least , is the theory of Mr. Charles Darwin , who thus explains the formation of atolls -- a theory superior , in my view , to the one that says these madreporic edifices sit on the summits of mountains or volcanoes submerged a few feet below sea level .

三亚水域造礁石珊瑚移植试验研究

A study on the transplantation of reef-building corals in Sanya waters , Hainan Province

晚三叠世造礁生物主要为珊瑚和藻类；中晚侏罗世以珊瑚礁与海绵礁为主。

The Late Triassic reef-building organisms are dominated by corals and algae , whereas the Middle and Upper Jurassic ones by coral reefs and sponge reefs .