【目的】海洋沉积物中的古菌在全球生物地球化学循环中充当重要的角色,深入了解沉积物中古菌群落的结构及功能特征是探究海洋沉积物中古菌参与生物地球化学循环和生态学功能的基础。【方法】采用高通量测序技术,分别对南海北部陆坡不同...【目的】海洋沉积物中的古菌在全球生物地球化学循环中充当重要的角色,深入了解沉积物中古菌群落的结构及功能特征是探究海洋沉积物中古菌参与生物地球化学循环和生态学功能的基础。【方法】采用高通量测序技术,分别对南海北部陆坡不同海域(东部,西部和神狐海域的7个站位)沉积物中古菌16SrRNA基因进行Illumina Mi Seq测序。【结果】中国南海北部陆坡沉积物中古菌的主要门类是Bathyarchaeota、Thermoplasmata、Woesearchaeota(DHVEG-6)、Thaumarchaeota(Marine Group I)、Lokiarchaeota和Marine Hydrothermal Vent Group(MHVG),还存在少量的AK8、Marine Benthic Group A和Terrestrial Hot Spring Crenarchaeota Group(THSCG)等。在潜在水合物区沉积物中还发现了甲烷代谢相关古菌(Anaerobic methanotrophic archaea,ANME)类群,主要为ANME-1、ANME-2ab和ANME-2c等。甲烷代谢古菌的分布特征也从甲烷代谢保守功能基因mcr A(Methyl coenzyme-Mreductase A)的扩增中得到了验证。利用定量PCR对南海沉积物中的细菌、古菌的16SrRNA基因和mcrA基因进行了定量,发现细菌16SrRNA基因拷贝数为10~5-10~7 copies/g(湿重),古菌16SrRNA基因拷贝数为10~5-10~6 copies/g(湿重),潜在水合物区mcrA基因拷贝数为10~3-10~5 copies/g(湿重)。【结论】揭示了中国南海北部陆坡沉积物中具有丰富的微生物资源,其中古菌种类多样且丰度较高,同时发现冷泉特征古菌群落,为深入认识和理解南海沉积物中微生物丰度和古菌多样性,以及解析古菌地球化学功能奠定基础。展开更多
BSR （Bottom Simulating Reflector） occurs widely in the strata since the late Miocene in the deep-water area of the northern continental slope of South China Sea （SCS）. It is an important seismic reference mark whi...BSR （Bottom Simulating Reflector） occurs widely in the strata since the late Miocene in the deep-water area of the northern continental slope of South China Sea （SCS）. It is an important seismic reference mark which identifies the gas hydrate and its distribution influenced by the tectonic movements. Single-point basin modeling was conducted using 473 points in the study area. To discuss the relationships between the tectonic subsidence and BSR, the volume and rate of tectonic subsidence in each geological time have been simulated. The results show that there are three tectonic accelerate subsidence processes in the study area since the late Miocene, especially since 1.8Ma the tectonic subsidence accelerates more apparently. Since the Late Miocene to Pleistocene, the rate of tectonic subsidence in deep-water underwent a transformation from weak to strong. The ratio of tectonic subsidence to the total subsidence was relatively high （65-70%）. Through the superposition of the BSR developed areas and the contours of tectonic subsidence in this area, it was discovered that more than 80% of BSR tend to be distributed at the slope break or depression-uplift structural transfer zone and the average tectonic subsidence rate ranges from 70 m/Ma to 125 m/Ma.展开更多
The shallow shelf delta/strand arenaceous-pelitic deposit region in the north of the Pearl River mouth basin, sitting on the northern continental shelf of the South China Sea, has already become an important oil produ...The shallow shelf delta/strand arenaceous-pelitic deposit region in the north of the Pearl River mouth basin, sitting on the northern continental shelf of the South China Sea, has already become an important oil production base in China. Recent researched has revealed that a great deal of deep-water fans of great petroleum potentiality exist on the Baiyun deep-water slope below the big paleo Pearl River and its large delta. Based on a mass of exploration wells and 2-D seismic data of the shallow shelf region, a interpretation of sequence stratigraphy confirmed the existence of deep-water fans. The cyclic falling of sea level, abundant detrital matter from the paleo Pearl River and the persistent geothermal subsidence in the Baiyun sag are the three prerequisites for the formation and development of deep-water fans. There are many in common between the deep-water shelf depositional system of the northern South China Sea and the exploration hotspots region on the two banks of the Atlantic. For example, both are located on passive continent margins, and persistent secular thermal subsidence and large paleo rivers have supplied abundant material sources and organic matter. More recently, the discovery of the big gas pool on the northern slope of the Baiyun sag confirms that the Lower Tertiary lacustrine facies in the Baiyun sag has a great potentiality of source rocks. The fans overlying the Lower Tertiary source rocks should become the main exploration areas for oil and gas resources.展开更多
文摘【目的】海洋沉积物中的古菌在全球生物地球化学循环中充当重要的角色,深入了解沉积物中古菌群落的结构及功能特征是探究海洋沉积物中古菌参与生物地球化学循环和生态学功能的基础。【方法】采用高通量测序技术,分别对南海北部陆坡不同海域(东部,西部和神狐海域的7个站位)沉积物中古菌16SrRNA基因进行Illumina Mi Seq测序。【结果】中国南海北部陆坡沉积物中古菌的主要门类是Bathyarchaeota、Thermoplasmata、Woesearchaeota(DHVEG-6)、Thaumarchaeota(Marine Group I)、Lokiarchaeota和Marine Hydrothermal Vent Group(MHVG),还存在少量的AK8、Marine Benthic Group A和Terrestrial Hot Spring Crenarchaeota Group(THSCG)等。在潜在水合物区沉积物中还发现了甲烷代谢相关古菌(Anaerobic methanotrophic archaea,ANME)类群,主要为ANME-1、ANME-2ab和ANME-2c等。甲烷代谢古菌的分布特征也从甲烷代谢保守功能基因mcr A(Methyl coenzyme-Mreductase A)的扩增中得到了验证。利用定量PCR对南海沉积物中的细菌、古菌的16SrRNA基因和mcrA基因进行了定量,发现细菌16SrRNA基因拷贝数为10~5-10~7 copies/g(湿重),古菌16SrRNA基因拷贝数为10~5-10~6 copies/g(湿重),潜在水合物区mcrA基因拷贝数为10~3-10~5 copies/g(湿重)。【结论】揭示了中国南海北部陆坡沉积物中具有丰富的微生物资源,其中古菌种类多样且丰度较高,同时发现冷泉特征古菌群落,为深入认识和理解南海沉积物中微生物丰度和古菌多样性,以及解析古菌地球化学功能奠定基础。
基金supported by the National 973 Basic Research Program (Grant No. 2009CB219502)National Natural Science Foundation of China (Grant No. 41072084)
文摘BSR （Bottom Simulating Reflector） occurs widely in the strata since the late Miocene in the deep-water area of the northern continental slope of South China Sea （SCS）. It is an important seismic reference mark which identifies the gas hydrate and its distribution influenced by the tectonic movements. Single-point basin modeling was conducted using 473 points in the study area. To discuss the relationships between the tectonic subsidence and BSR, the volume and rate of tectonic subsidence in each geological time have been simulated. The results show that there are three tectonic accelerate subsidence processes in the study area since the late Miocene, especially since 1.8Ma the tectonic subsidence accelerates more apparently. Since the Late Miocene to Pleistocene, the rate of tectonic subsidence in deep-water underwent a transformation from weak to strong. The ratio of tectonic subsidence to the total subsidence was relatively high （65-70%）. Through the superposition of the BSR developed areas and the contours of tectonic subsidence in this area, it was discovered that more than 80% of BSR tend to be distributed at the slope break or depression-uplift structural transfer zone and the average tectonic subsidence rate ranges from 70 m/Ma to 125 m/Ma.
基金This study was supported by the project“the deep-water fan systems and petroleum resources in the South China Sea”(grant 40238060)sponsored by the Natural Science Foundation of China and the China National Offshore Oil Corporation.
文摘The shallow shelf delta/strand arenaceous-pelitic deposit region in the north of the Pearl River mouth basin, sitting on the northern continental shelf of the South China Sea, has already become an important oil production base in China. Recent researched has revealed that a great deal of deep-water fans of great petroleum potentiality exist on the Baiyun deep-water slope below the big paleo Pearl River and its large delta. Based on a mass of exploration wells and 2-D seismic data of the shallow shelf region, a interpretation of sequence stratigraphy confirmed the existence of deep-water fans. The cyclic falling of sea level, abundant detrital matter from the paleo Pearl River and the persistent geothermal subsidence in the Baiyun sag are the three prerequisites for the formation and development of deep-water fans. There are many in common between the deep-water shelf depositional system of the northern South China Sea and the exploration hotspots region on the two banks of the Atlantic. For example, both are located on passive continent margins, and persistent secular thermal subsidence and large paleo rivers have supplied abundant material sources and organic matter. More recently, the discovery of the big gas pool on the northern slope of the Baiyun sag confirms that the Lower Tertiary lacustrine facies in the Baiyun sag has a great potentiality of source rocks. The fans overlying the Lower Tertiary source rocks should become the main exploration areas for oil and gas resources.
