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在澳大利亚南部一处新发现的土伦阶(约9000万年前)琥珀中保存的生物内含物和假内含物的范围。

The range of bioinclusions and pseudoinclusions preserved in a new Turonian (~90 ma) amber occurrence from Southern Australia.

作者信息

Quinney Annie, Mays Chris, Stilwell Jeffrey D, Zelenitsky Darla K, Therrien François

机构信息

School of Earth, Atmosphere & Environment, Monash University, Clayton, Victoria 3800, Australia.

Department of Geoscience, University of Calgary, Calgary, Alberta, T2N 1N4 Canada.

出版信息

PLoS One. 2015 May 13;10(5):e0121307. doi: 10.1371/journal.pone.0121307. eCollection 2015.

Abstract

A new Turonian amber occurrence, representing the oldest in situ amber locality in Australia and the southern-most locality in Gondwana, has recently been discovered in the Otway Basin of Victoria. The amber was collected from petroleum cores and many pieces contain a range of inclusions that can provide information on the depositional history of the resin. To date, one species of fern spore (Cyathidites minor) and one species of lycophyte spore (Kraeuselisporites sp?) have been conclusively identified in the amber, along with filamentous microorganisms and degraded plant matter. Several samples are also rife with pseudoinclusions as reported recently in other ambers. The abundance of preserved particulate debris and wind dispersed spores suggest that the Otway amber formed subaerially. Furthermore, based on the range of bioinclusions and forms of pseudoinclusions preserved within a single piece of amber, the locus of hardening for individual samples is variably interpreted as occurring in the tree tops, on the tree trunk or on the ground surface. Notably, specific inclusion assemblages are associated with certain colours of amber. By extension, and in accordance with recent studies, amber colour may be indicative of depositional environment. Variation in the environment of solidification may, therefore, be sufficient to account for the broad range of morphological characteristics preserved in a single amber deposit.

摘要

在维多利亚州的奥特韦盆地,最近发现了一处新的土伦阶琥珀产地,它代表了澳大利亚最古老的原地琥珀产地以及冈瓦纳最南端的产地。这些琥珀是从石油岩芯中采集的,许多碎片包含一系列内含物,能够提供有关树脂沉积历史的信息。迄今为止,在琥珀中已确凿鉴定出一种蕨类植物孢子(小桫椤孢)和一种石松类植物孢子(克氏孢属?),还有丝状微生物和降解的植物物质。正如最近在其他琥珀中所报道的那样,几个样本中也充斥着假内含物。大量保存下来的颗粒碎片和随风散布的孢子表明,奥特韦琥珀是在陆地上形成的。此外,基于保存在一块琥珀中的生物内含物范围和假内含物形式,单个样本的硬化位置被不同地解释为发生在树顶、树干或地面。值得注意的是,特定的内含物组合与特定颜色的琥珀相关。因此,根据最近的研究推断,琥珀颜色可能指示沉积环境。固化环境的变化可能足以解释保存在单个琥珀矿床中的广泛形态特征。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e7cf/4430482/3b7caddbccbf/pone.0121307.g001.jpg

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