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The δ^13C and Mg/Ca curves drawn from the investigated stalagmites mostly follow the fluctuation of regional paleotemperature, but may be overprinted by other climatic signals.

从研究的石笋中所提出的δ^13C与Mg/Ca曲线一般随区域古气温波动而变化,但不能排除其中有另类气候信号的叠加。

The gaps between stalagmites equally grew from sparse to dense, which was hard to detect in the eyes, until eventually they formed a passageway lined by two stonewalls.

石笋同样以眼睛难以觉察的距离逐渐由疏到密,最后组成了两堵石墙夹成的通道。

Finally, the drop water is supersaturating to carbonate and then the CaCO_3 sediment.

因此在现代石笋古气候研究中,机理研究和古气候序列的建立并重。

Comparison of the same Southwest monsoonal climate areas and the same study period with Dongge Cave and Kahf Defore Cave in δ18O values, the tufa core of δ18O in Huanglong is higher extent than these of Cave records, which altitude effect and different removal of moisture source regions maybe lead to extent difference in δ18O values; and we can draw a conclusion the tufa core records of Huanglong in the high altitude and middle latitude areas is more sensitive respond to climatic environmental changes than records of stalagmites in Dongge Cave and Kahf Defore Cave from the low altitude areas.

同属西南季风区、由于海拔效应和距离水汽来源远近不同等因素的影响,在同时段内黄龙钙华δ18O 的变化范围和变化幅度都比董歌洞和Kahf Defore 洞的δ18O记录要大,说明处于中纬度、高海拔的黄龙钙华相对于低海拔的董歌洞和Kahf Defore洞石笋对气候环境的响应可能更加敏感。

Exquisite stalactite cave, stalagmites,石幔, stone shield silver, beautiful, especially that of the goose Jingying translucent tubes, sticks of rock curly, white transparent crystal stone, stone flower long-haired, wearing a rock formed a unique the four characteristics of high value ornamental and scientific research.

洞内精美的石钟乳、石笋、石幔、石盾琳琅满目,美不胜收,特别是那晶莹透亮的鹅管、卷曲的石枝、雪白透明的水晶石、石头开花长毛,形成了穿山岩独有的四大特色,具有很高的观赏和科研价值。

Approximately 30,000 years ago, long on stable sand dune plant root, passes through the long time the decency, has formed the limestone, after the plant dies, the sand dune unceasing migration, causes these calcifications the limestone to reveal the surface, has formed the stalagmite which the present sees.

大约在3万年前,长在稳定的沙丘上的植物根部,经过长时间的风化,形成了石灰岩,植物死后,沙丘的不断移动,使这些钙化的石灰岩露出地表,形成了现在所看到的石笋

In the cave, there are piles of stalactites and stalagmites in curious shapes such as wild beasts and human figures which look like corals, ambers and jades under the coloured lights.

洞内有许多钟乳石和石笋,形状奇异,在彩色灯光下,像珊瑚,琥珀和玉石。它们的形状有的像猛兽,有的像人物。

Round about, pile of lime—stone glistened in all the colours of the rainbow

在寂静得可怕的洞穴,唯一能听到声音是从石笋顶部不断往下滴的水滴声

One from the growth of stalactite-down, bottom-up, said the growth of stalagmites.

其中由上向下生长的石钟乳,由下向上生长的称石笋

Thanks to Van Zyl, today the public can enjoy the sight of magnificent stalactites and stalagmites.

由于他的发现,我们今天才欣赏到了美丽的钟乳石和石笋

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