基于化学合成群落进化生态学的热液活动历史估算

S. Kojima, H. Watanabe, K. Fujikura
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引用次数: 1

摘要

在深海还原性环境中,如热液喷口区和冷渗区,经常观察到具有巨大生物量的生物群落。这些与细菌化学合成有关的群落是由这些环境特有的物种组成的,它们是在热液活动中建立的,并随着活动的变化而成功。在更长的时间尺度上,在一系列活动过程中,局部种群和物种形成之间发生遗传变异,最终产生新的动物群。在“针叶林项目”的基础上,基于热液喷口特有动物的进化生态学,我们试图在10 ~ 107年的不同时间尺度上估计各种热液现象的年龄。本文介绍了热液喷口地区的生物群落,并描述了我们正在规划的年龄估计方法的原理和预期结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of History of Hydrothermal Activities Based on Evolutionary Ecology of Chemosynthesis-based Communities
In deep-sea reducing environments, such as hydrothermal vent fields and cold seep areas, biological communities with huge biomass are often observed. Such communities associated with bacterial chemosynthesis, which are composed of species endemic to these environments, are founded with hydrothermal activities and succeed with changes of activities. Over a longer timescale, genetic deviations among local populations and speciation occur during the course of a series of activities and finally new faunal groups diverged. We attempt to estimate the ages of various hydrothermal phenomena on various timescales from 10 to 107 years on the basis of the evolutionary ecology of animals endemic to hydrothermal vents as part of the “Taiga project”. In this paper, we introduce communities in hydrothermal vent fields and describe the principals of methodologies for age estimation, which we are now planning, and the expected results.
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