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Cryptic bioentities with their significance from the Gotan Formationof Bilara Group, Marwar Supergroup, Rajasthan

机译:隐秘生物实体及其意义,来自拉贾斯坦邦Bilara组,Marwar Supergroup组,Gotan组

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The Neoproterozoic (1000–542 Ma) period is recognized as the most significant in the earth’s history basing on the available information from the different studies, including physical and biological factors. The plate motion is coherent with complexgeodynamics, responsible for the opening up of new oceans and closing others (ecospace) due to break-up and amalgation/subsidence of the crustal blocks in the Gondwana Supercontinent1,2. There are negligible chances of preservation of molecular and cellbiological characters, except structural bioentities in that condition3. The explosion and diversification of the acritarchs including morpho-complex fossils (planktic and benthic) are celluloid/ biomineralized forms, burried/preserved in the sedimentsand on the bedding planes of rocks. In Precambrian micropalaeontology, the acritarchs and algae are considered as important and second most significant key tool after molecular remnants. Hence they are used by various workers (see cited references therein)4 for biostratigraphy and age implications for complex geological successions in the absence of dating minerals as well as palaeoenvironment. The evolution of the new progeny in algae is the result of the interplay of many diverse genes subjected to little morphological changes without disturbing the genotype by spatial gene. These genes act as autotransformations with regular intervals in algae rather than environmental condition.
机译:根据不同研究的可用信息,包括物理和生物学因素,新元古代(1000-542 Ma)时期被认为是地球历史上最重要的时期。板块运动与复杂的地球动力学相一致,由于冈瓦纳超大陆1,2地壳块的破裂和融合/沉陷,造成了新海洋的开放和其他海洋(生态空间)的封闭。除了在那种条件下的结构生物实体外,保留分子和细胞生物学特性的机会微乎其微。包括形态复杂化石(浮游生物和底栖生物)在内的头颅的爆炸和多样化是赛璐ul /生物矿化的形式,埋藏/保留在沉积物中和岩石的层理平面上。在前寒武纪微古生物学中,除贝壳状藻和藻类是重要的工具,也是仅次于分子残留物的第二重要的关键工具。因此,在没有定年矿物和古环境的情况下,各种工作者(参见其中引用的参考文献)4将它们用于复杂的地质演替的生物地层学和年龄意义。藻类中新后代的进化是多种多样的基因相互作用的结果,这些基因几乎没有受到形态学变化的影响,而不会干扰空间基因的基因型。这些基因在藻类中而不是环境条件下以规则的间隔充当自体转化。

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