据215篇有关江山的古生物学、地层学研究成果，简述了浙江江山古生物地层的研究历史。
According to 215 papers of palaeontology and stratigraphic geology from Jiangshan, Zhejiang, the history of palaeontology and strata from Jiangshan, Zhejiang is briefly introduced.
然而，这个7亿年历史的地层几乎不能为现代动物的起源提供任何线索，因为古生物学家认为它代表的是一个失败的进化试验。
This 700-million-year-old formation gives few clues to the origins of modern animals, however, because paleontologists believe it represents an evolutionary experiment that failed.
“如果火星上有足够的生命形成地层，珊瑚或某种微生物，并且被掩埋，那么，发生在地球上的物理现象或许也发生在火星上”，他说。
"If there was enough life to make layers, to make corals or some sort of microbial homes, and if it was buried on Mars, the same physics that took place on Earth could have happened there," he said.
结果表明，盆地周边岩石、煤系地层为富砷岩系，构成砷的原生物源。
The study indicates that the arsenic rich rocks around the basin and coal series strata are the original arsenic sources.
本组为评估中元古代生命状况、古环境和前显生宙生物地层提供了重要的生物信息。
This Formation provides important paleobiological information from which to assess status of Mesoproterozoic life, and to evaluate paleoenvironmental conditions and pre_Phanerozoic biostratigraphy.
贵州省关岭县新铺乡附近的晚三叠世早期地层瓦窑组底部产具重大科学意义的关岭生物群。
The Guanling biota, which has important scientific significance, has been found at the bottom of the early Late Triassic Wayao Formation near Xinpu Township, Guanling County, Guizhou Province.
羌南地区奥陶纪—泥盆纪生物和地层的发现，为与邻区地层划分对比和探讨羌塘构造演化提供了重要依据。
The discovery of Ordovician-Devonian biotas and strata provide new important evidence for the stratigraphic division and correlation and the study of the tectonic evolution of the Qiangtang area.
概要的总结了东北区中生代地层中古生物群，以及它们在岩石地层单位中的分布，借以说明岩石地层的时代，为地层多重划分对比提供了依据。
The Mesozoic biota and their distribution in lithostratigraphic units in northeastern China are summed up to suggest the age of the units and to be the basin for multiple classification of strata.
从轮藻角度讲，中国当阳跑马岗组的白垩-古近系过渡段的生物地层记录是世界上迄今所知的最连续和最丰富的。
From the point of view of charophytes, the biostratigraphic records from the Paomagang Formation in Dangyang (China) are most continuous and abundant known so far in the world.
然后从沉积微相分析入手，研究了沉积相标志，包括地层岩石的颜色、沉积构造、粒度分布、古生物学等。
Then, beginning with the microfacies, signs of sediment facies, including rock's colour, sediment structure, granularity distribution, fossil and so on, are studied.
重质稠油藏的形成主要受盆地后期抬升活动、生物降解、地层水洗和氧化作用等因素控制。
The formation of heavy oil reservoirs is chiefly controlled by late uplifting of the basin, biodegradation, water-washing, and free oxygen oxidizing.
在巨蛇的化石旁边，研究人员还发现了一种和鳄鱼类似的生物的化石。这是首次从塞雷洪地层发现鳄形目的生物。
Remains of the croc-like animal were found close to the imposing snake. It's the first ever crocodyliform to be identified from the site, the Cerrejon Formation.
本文为我国首次采用生物地层法探讨西太平洋麦哲伦海山区富钴结壳的生长年代。
The age of cobalt-rich crusts from the Magellan Seamount in the western Pacific has been first approached by using the method of biostratigraphic dating.
采取点、线、面相结合， 岩石地层学、 生物地层学和同位素年代学相结合的工作方法，研究了这套地层的层序、划分和对比问题；
The succession, division and correlation of these strata are studied with lithostratigraphy, biostratigraphy and isotopic geochronology methods and by the combination of of point, line and area.
地层古生物、区域岩石及地质构造、地质灾害、矿产资源及旅游地学等方面取得较多的新成果和新认识。
Many new results and new knowledge in stratigraphy, palaeontology, regional lithology and tectonics, geological disaster, mineral resources and tourist geoscience.
通过生物地层、年代地层、岩石地层的研究，对四川盆地二叠系进行重新划分。
With study on biological stratigraphy, geochron stratigraphy, and lithologic stratigraphy, Permian is re-divided in Sichuan Basin.
该地体的地层古生物、岩石以及构造特征完全与日本列岛的美浓地体相同。
Paleontological and petrological characteristics and structural features of these formations are entirely identical to those of the Mino terrane of the Japanese Islands.
综合评价微生物采油现场试验研究及试验效果，讨论微生物在地层中的生长繁殖、运移及提高采收率机理。
The pilot test result of MEOR was evaluated and the reproduction, breeding and migration of micro organism in strata, and the MEOR's mechanism were discussed.
本文研究工作的重点集中在地层古生物学、沉积岩石学研究两大方面。
Thepresent work is mainly focus on the paleontology and sedimentology, as well as the lithology.
本文概略地介绍了近十年来，贵州在地层古生物、构造地质、沉积地质及岩浆岩等基础地质方面取得的新进展。
The paper outlines the new progress of basic geology, such as stratigraphy, palaeontology, tectonic geology, sedimentary geology and magmatic rock, for last ten years.
由于地层的连续和生物化石研究的深入，已经具备了探讨当时海洋溶解氧变化与生物演化特征的条件。
Detailed research on stratigraphy and paleontology has provided the conditions for discussing the Marine dissolved oxygen variations and organic evolvements.
生物地层学是地层学中最基本的也是应用最广泛的一个分支学科。
Biostratigraphy is one of the basic and widely applied branches in stratigraphy.
地层中生活着成千上万种微生物，但是只有一些特定的微生物种群与碳氢化合物保持着密切的关系。
There are hundreds of thousands of different microbes living inside a formation but certain species are associated with hydrocarbons tend to stand out.
本文系统研究了西昆仑-喀喇昆仑地区晚古生代-早中生代地层的岩石组合及其分布特征，结合所含的生物组合特征绘制了研究区泥盆纪、石炭纪、早中二叠世及三叠纪的岩相古地理略图。
The late Paleozoic-early Mesozoic strata in the Western Kunlun-Karakorum area are main research object and the accreting orogenic theory is used for structural analysis in this paper.
室内研究证明在大庆油田选择性地激活地层中的本源微生物采油菌，可以有效地提高油藏采收率。
Lab study has proved that selective activation of authigenous microorganism oil production bacteria in the formation in Daqing Oilfield can effectively enhance oil recovery.
地一层层堆积起来，跟外界空气隔绝着，经过细菌的分解，以及地层内的高温、高压作用，生物遗体逐渐分。
They piled and were separated from the air. Germs decomposing the bodies, along with the high temperature.
山东诸城是我国研究白垩纪地层和古生物的经典地区之一，特别以产出晚白垩世鸭嘴龙类恐龙化石群而闻名中外。
Zhucheng City of Shandong Province is one of classic areas for the study on Cretaceous strata and fossils in China, yielding rich Late Cretaceous hadrosaurid dinosaurs famously.
养分是原油生物降解的最终控制因素，在没有明显地层水活动的区带，底水存在与否及底水层厚度大小就成了生物降解的另一个重要控制因素。
Nutrient is the terminal controlling factor. At the area of no obvious formation water, the occurrence and thickness of bottom water are the other important factors.
石油是远古时代生物的遗体在地层中经过几亿年的变化而逐渐形成的。
Oil is the remains of ancient organisms in formation through the hundreds of millions of years of evolving changes.
石油是远古时代生物的遗体在地层中经过几亿年的变化而逐渐形成的。
Oil is the remains of ancient organisms in formation through the hundreds of millions of years of evolving changes.
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