this paper studies on the subject of national 863 project – 7000 meters manned submersible special task ( the target recognition technique of undersea hydrothermal vent image).

our results move us a step closer towards understanding the evolutionary origin of hydrothermal vent species and their distribution in the western pacific-indian ocean region.

我们的结论加深了人们对海底热液口的生命起源与进化及其在西太平洋和印度洋的分布的理解。

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life activity and biological populations have been found recently in areas of hydrothermal vent and metallic sulfide deposits, which is of great significance in science.

在高温热液活动区及金属硫化物沉积中发现大量生命活动和生物群体，意义重大。

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the culture of micro-oxygen demanding and baroduric bacteria from a deep-sea hydrothermal vent

深海热液喷口周围微氧耐压细菌的培养研究

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basing on this analysis, this paper developed an adaptive algorithm for undersea hydrothermal vent image.

在此基础上，设计了一种海底热液图象的自适应分割方法。

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hydrothermal vent ecosystem and cold seep community of deep sea

深海洋底热泉生态系和冷泉生物研究综述

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research advances in hydrothermal vent microbial communities and its significance for geology

现代海底热液微生物群落及其地质意义

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research advances in deep-sea hydrothermal vent communities

深海热液喷口生物群落的研究进展

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adaptive segmentation algorithm for undersea hydrothermal vent image.

海底热液喷口图象的自适应分割方法研究。

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and there's another technique that's been experimented with to try to help coral reefs recover from bleaching.

人们还尝试了另一种技术，试图帮助珊瑚礁从漂白中恢复。

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remote sensing technology can provide sst and ocean color data with large coverage in both space and time, and sst data can be applied in monitoring and forecasting coral bleaching.

卫星遥感能够提供大范围、同步与连续的海洋数据，如海水表层温度和海色数据，从而能够及时监测和预测珊瑚礁的白化。

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now that the vote has been done, we'll see a few years of site sampling to figure out the best global standard stratigraphic age ( gssa) to date the start of the anthropocene, which will then be presented to the international commission on stratigraphy.

纪元变更的投票结束后，工作组在未来几年会利用现场勘测数据计算出最佳的全球标准低层年龄（GSSA），并确定“人类世”的开始日期，届时会把研究结果呈递国际地层委员会。

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on our species' impact on the planet. "the anthropocene works as a geological unit of time, process and strata," zalasiewicz told nature.com. "it is distinguishable. it is distinctive."

扎拉塞维奇告诉自然杂志网站说：“人类世是时间、过程和地层的地质单位。它是可辨别的，也是独特的。”

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the anthropocene is different. it is one of those moments where a scientific realisation, like copernicus grasping that the earth goes round the sun, could fundamentally change people's view of things far beyond science.

人类纪就不一样了，像哥白尼掌握了地球围绕太阳运转那样，它是科学认识可以从根本上改变人们对远远超乎科学事物看法的时刻。

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last week, a panel of scientists voted in favor of classifying the age we are living in as a new geological epoch-the "anthropocene"-after reviewing available evidence on the issue.

上周，一组科学家在审阅了现有证据之后，投票赞成将我们所处的时代划分为一个新的地质时代——人类世。

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rather than placing us still in the holocene, a peculiarly stable era that began only around 10000 years ago, the geologists say we are already living in the anthropocene: the age of man.

地质学家们称，我们已经生活在人类纪——人的时代，而不是仍将人类放在约1000年前开始的特别稳定的年代——全新世。

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although farms have changed the world for millennia, the anthropocene advent of fossil fuels, scientific breeding and, most of all, artificial nitrogen fertiliser has vastly increased agriculture's power.

尽管农业改变世界已有千年历史，人类纪出现的化石燃料、科学繁殖以及最重要的人工氮肥极大地加大了农业的力量。

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the 11700-year-old geological holocene epoch has ended, scientists say, and we're now living in the anthropocene: an era defined by humanity's influence on the world around us.

如今，地质学界打算用地质术语来确认这些影响。科学家表示，长达11700年的全新世已结束，我们现在正生活在“人类世”：即人类活动对地球施加影响的时代。

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although the technologies are still nascent, the idea that humans might help remove carbon from the skies as well as put it there is a reasonable anthropocene expectation;

尽管技术尚不成熟，人类可能从天空去除碳，也能将碳放到天空这一想法可能是合理的人类纪展望。

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and that's the kind of techno-fossil that may prove to be a hallmark of the anthropocene age, this time of humanity shaping the planet.

而就是这种技术导致的化石类物质也许能作为地球人类时代存在过的标记，我们人类影响着自己所生活的这颗星球。

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the challenge of the anthropocene is to use human ingenuity to set things up so that the planet can accomplish its 21st-century task.

人类纪的挑战在于运用人类智慧让地球能够完成21世纪的任务。

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