Non-marine carbonate: Wherefore art thou?

IF 1.9 3区 地球科学 Q1 GEOLOGY
Enrico Capezzuoli, Giovanna Della Porta, Mike Rogerson, Ezher Tagliasacchi
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引用次数: 2

Abstract

Introduction of the special issue on non-marine carbonates. (A) Sub-lacustrine spring pinnacles from alkaline Mono Lake (California, USA); scale is 2 m. (B) Cascade tufa from Sarikavak (TK); scale is 175 cm. (C) Travertine deposits from Pamukkale (TK); scale is 170 cm. (D) Speleothems and flowstones from Kaklık Cave (TK); hammer for scale. (E) Temporarily exposed microbial bioherms at Bridger Bay shoreline, Antelope Island, Great Salt Lake (Utah, USA); sedimentologists for scale. (F) Upper Jurassic rhizolite laminar calcrete (base at hammer edge) from Rochaforte (Portugal; courtesy of V.P. Wright; Wright & Azerêdo, 2006). (G) The Brook Bottom leachate deposit (Harpur Hill, Derbyshire, UK). Anthropocene carbonate deposit forming downstream of a legacy deposit of impure lime, left by historical industrial activity at the site (courtesy of Laura Bastianini); scale is about 10 m.

Abstract Image

非海相碳酸盐:你为什么?
尽管众所周知很难从更广泛的碳酸盐岩和沉积物家族中进行描述,但非海相碳酸盐岩是一个重要的亚群,形成于各种沉积环境中,如湖泊、河流、热液喷口、洞穴,受碱性污染影响的土壤和场地(Alonso-Zarza&Tanner,2010;Capezzuoli等人,2014;Della Porta,2015;五旬节,2005年;图1)。由于大气降水在陆地环境中的侵蚀和溶解作用,这些碳酸盐岩通常具有较低的保存潜力,其地质记录可能是不连续和高度蚀变的。然而,非海相碳酸盐岩是陆地沉积盆地的重要组成部分,为古环境条件提供了有用的指标,并可以为受人类工业危害的地点提供被动修复的手段,包括二氧化碳的封存和储存。了解其降水过程中涉及的物理化学和微生物介导的过程有助于限制生物地球化学循环,调查地质过去,并规划未来应对全球变化的方法。在过去的二十年里,非海相碳酸盐岩的研究从对局部事件的描述发展到了前沿研究,能够涵盖最新的具有挑战性的兴趣,如地球生命的黎明或天体生物学研究(包括Des Marais和Walter,2019;Farmer,2000;Franchi和Frisia,2020;Rothschild和Mancinelli,2001),并已成为未来地球工程研究的主要目标。本特刊旨在开始收集和策划必要的知识,以解决这一前沿研究面临的挑战。我们需要更好地了解非海相碳酸盐相的多样性,以及对碳酸盐和相关矿物沉淀过程的物理化学和生物成因控制,以使我们的研究超越对所发生情况的观察,重建时间和空间过程。收集到的资料通过多学科方法研究了化石和现代非海相碳酸盐岩,强调了它们在不同沉积环境和年龄之间的可变性,以及控制其形成、组构和堆积速率的生物、环境和化学因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
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