1)  pateobiochemistry
古生物化学
2)  Palaeo biochemistry
古生物化学
3)  Early Paleozoic
早古生代
1.
Early Paleozoic palaeogeomorphology—characteristics of slope break zones and their control on stratigraphic-lithologic traps in Tarim Basin;
塔里木盆地早古生代古地貌——坡折带特征及对地层岩性圈闭的控制
2.
Chemical mobility of selenium in early paleozoic rock and stone coal in Daba Mountain, South Qinling;
大巴山区早古生代地层和石煤中硒的化学活动性的初步研究
3.
Discovery of Early Paleozoic granites in the eastern Xiao Hinggan Mountains, northeastern China and their tectonic significance;
小兴安岭东部早古生代花岗岩的发现及其构造意义
4)  Lower Paleozoic
下古生界
1.
Oil-gas exploration prospect of dolomite reservoir in the Lower Paleozoic of Tarim Basin;
塔里木盆地下古生界白云岩储层油气勘探前景
2.
The Characteristics of Fluid Inclusions in Lower Paleozoic System of the Well Wuke 1 and the Analysis of the Reservoir-forming Stage;
五科1井下古生界流体包裹体特征与天然气成藏期分析
3.
The forming mechanism of dolomite reservoir space of Lower Paleozoic in Zhuanghai region, Jiyang Depression;
济阳坳陷桩海地区下古生界白云岩储集空间形成机理
5)  Paleozoic erathem
古生界
1.
Analysis of high-resolution sequence stratigraphy and coal accumulation law of upper Paleozoic erathem in Ordos Basin;
鄂尔多斯盆地上古生界高分辨率层序划分与煤聚积规律分析
2.
The enormous amount of natural gas generated from gas source rock of Paleozoic erathem and continuous gas supply ability is the base of the concertrated gas reservoirs.
上古生界气源岩巨大的排气量和持续的供气能力是古生界气藏富集的基础 ,天然气早期以垂向和侧向运移为主 ,晚期就近运移聚集 ,为古生界特别是上古生界大面积含气提供了有利条件。
3.
From on production in 1997 to 2002, Paleozoic Erathem carbonate-rock gas pool in Changqing gas field has built up accumulative production capacity of 39.
长庆靖边下古生界碳酸盐岩气藏自1997年投产以来,到2002年底已累计建成年产39。
6)  Paleozoic
古生代
1.
Review and revelation of oil/gas discoveries in the Paleozoic marine strata of China;
中国古生代海相油气田发现的回顾与启示
2.
Re-discussion on exploration potential of Paleozoic in Tarim basin: 20 thanniversary of significant discovery in Shacan 2 well;
再论塔里木盆地古生代油气勘探潜力——纪念沙参2井油气重大突破20周年
3.
Metallogenic regularity of Qinling-Qilian-Kunlun metallogenic domain in Paleozoic;
秦祁昆成矿域古生代区域成矿规律
参考词条
补充资料：古生物化学
分子式：
CAS号：

性质：以化石中所含有机成分为研究对象，古生物学与生物化学相结合的新兴边缘学科。它是根据生物硬体形成化石后，岩石及化石中都有残留有机物，可利用现代精密分析技术手段，从各种各样的化石中分析出氨基酸、蛋白质。脂肪酸等各种有机成分，按照化石有机成分的含量和种类，可用于地层的划分和对比，并可通过系统的分析研究，探索地质历史时期生物有机成分的演变规律，从而进一步研究古生物的分类系统和亲缘关系，并为探索生命起源和分析古环境等提供依据。

说明：补充资料仅用于学习参考，请勿用于其它任何用途。