据古耶特称，储碳过程并不久远，甚至持续到今天因为不断有更多的树生长在水面下。
This carbon storage process is not just ancient; it continues even today as additional trees become submerged, according to Guyette.
受潜水面阶段性上浮，相对高的古地貌上发育多期次岩溶洞穴系统。
Phased by diving surface rise, relatively high paleogeomorphology developed karst cave system in many times.
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