生物的起源自生沸石-地球科学堆栈交换江南电子竞技平台江南体育网页版 最近30从www.hoelymoley.com 2023 - 04 - 26 - t20:18:19z //www.hoelymoley.com/feeds/question/272 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/272 10 生物的起源自生沸石 plannapus //www.hoelymoley.com/users/87 2014 - 04 - 17 - t11:09:06z 2014 - 11 - 15 - t14:27:10z < p > <强> Bohrmann et al . 1989 < / >强大先进的硅酸盐一些斜发沸石来自成岩阶段生物退化蛋白石(从放射虫在这种情况下也可能其他硅质化石)。< / p > < p >如果这个假设仍视为有效,斜发沸石是唯一的自生沸石可以追溯到生物蛋白石?< / p > < p >有任何域,因为本文的工作完成吗?< / p > < p > <子> <子>来源:< br > Bohrmann, G。斯坦,R。、Faugeres J.-C。,1989年。< a href = " http://dx.doi.org/10.1007/BF01829322 " rel =“nofollow”>自生硅沸石及其关系在ODP网站661沉积物成岩作用(108年腿,赤道东大西洋)< / >。Geologische优异,78 (3):779 - 792。< /子> < /订阅> < / p > //www.hoelymoley.com/questions/272/-/2805 # 2805 2 答案由user889生物起源自生沸石 user889 //www.hoelymoley.com/users/0 2014 - 11 - 15 - t14:27:10z 2014 - 11 - 15 - t14:27:10z < p >是的,有最近的研究在这个领域。本文< / p > < p > < a href = " http://www.pnas.org/content/96/7/3380.full.pdf " rel =“nofollow”>海洋矿物质:他们的起源、自然的环境中,和意义< / > (Kastner, 1999),他断言,< / p > < blockquote > < p >沸石钙十字沸石和方沸石主要反映火山物质的成岩作用;<强> clinoptilote和片沸石发生在制备了成岩环境。< /强> < / p > < /引用> < p >并确认< / p > < blockquote > < p >除了成岩opal-CT和石英形成生物opal-A解散的,其他常见的自生矿物硅酸铝蒙脱石和沸石。< / p > < /引用>

This is further confirmed by a 2007 paper Clinoptilolite as a new proxy of enhanced biogenic silica productivity in lower Miocene carbonate sediments of the Bahamas platform: Isotopic and thermodynamic evidence (Karpoff et al) which determined that

Seawater–rock modeling specifies that clinoptilolite precipitates from the dissolution of biogenic silica, which reacts with clay minerals. The amount of silica (opal-A) involved in the reaction has to be significant enough, at least 10 wt.%, to account for the observed content of clinoptilolite occurring at the most zeolite-rich level. Modeling also shows that the observed amount of clinoptilolite (∼ 19%) reflects an in situ and short-term reaction due to the high reactivity of primary biogenic silica (opal-A) until its complete depletion.

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