| FENG Jun,LI Jianghai,CHU Fengyou.A study of the microbial mineralization in submarine black smoker chimneys from the Okinawa Trough[J].Acta Oceanologica Sinica,2009,(2):87-95 |
| A study of the microbial mineralization in submarine black smoker chimneys from the Okinawa Trough |
| A study of the microbial mineralization in submarine black smoker chimneys from the Okinawa Trough |
| 投稿时间：2008-01-20 修订日期：2008-03-29 |
| DOI： |
| 中文关键词: microfossils biomineralization black smoker Okinawa Trough |
| 英文关键词:microfossils biomineralization black smoker Okinawa Trough |
| 基金项目:The Joint Seismological Research Fund under contract No.A07113. |
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| 中文摘要: |
| Large amounts of microfossil records discovered in the seafloor black smoker chimney are reported from the Okinawa Trough. They are well preserved and can be divided into four types of filamentous microfossils. It suggests that the fossils may be derived from sulfur or iron oxidation chemolithotrophic prokaryotes and fungi. Based on the comparison studies of the microbial mineralization processes, two steps of biomineralization were hypothesized:(1) biology controlled mineralization; and (2) biology induced mineralization. At the early stage of the mineralization, the biology controlling mineralization is dominating; at the later stage, the biology inducing mineralization is the main mechanism. The composition of the fluids and the species of the microbes will determine the types of the minerals formed. |
| 英文摘要: |
| Large amounts of microfossil records discovered in the seafloor black smoker chimney are reported from the Okinawa Trough. They are well preserved and can be divided into four types of filamentous microfossils. It suggests that the fossils may be derived from sulfur or iron oxidation chemolithotrophic prokaryotes and fungi. Based on the comparison studies of the microbial mineralization processes, two steps of biomineralization were hypothesized:(1) biology controlled mineralization; and (2) biology induced mineralization. At the early stage of the mineralization, the biology controlling mineralization is dominating; at the later stage, the biology inducing mineralization is the main mechanism. The composition of the fluids and the species of the microbes will determine the types of the minerals formed. |
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