美国印第安纳州 "纸 "煤中的卡林蝶化石切片(中宾夕法尼亚翼手目)。

IF 5.6 2区 工程技术 Q2 ENERGY & FUELS
José A. D'Angelo , James C. Hower , Gerardo Camí
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引用次数: 0

摘要

首次从卡林蝶(Karinopteris sp.)(中宾夕法尼亚时期的蝶形花)的喙中分离出一种类似角质素、具有高度耐化学腐蚀性的大分子聚合物。样本取自美国印第安纳州中西部帕克县的巴西地层上块煤层中的角质层或 "纸质 "煤页岩,即富含有机质和高度碎屑的岩石。Karinopteris 标本以自然氧化压缩的形式保存,被称为 "角质化石",可能代表了矿物基质环境中的植被。通过实验室氧化反应,我们获得了鞘翅目植物的角质层化石。经过额外和长期的氧化处理后,角质层产生了类似角质素的大分子聚合物,为简便起见,此处称为 "角质素"。利用半定量傅立叶变换红外光谱(FTIR)对卡林蝶的角质层化石、角质层和角质素样本进行了化学分析。Karinopteris rachises 的角质层红外光谱具有以下特征:(a)主要是脂肪族成分,在 3000-2700 cm-1 处有强烈的脂肪族(CHal)CH 伸展峰,这些峰归属于亚甲基(CH2)和甲基(CH3)基团;(b)在 1730-1640 cm-1 处有羰基(C=O)基团,在 1600-1500 cm-1 处有芳香族碳(C=C)吸收带。与角质层相比,角质层的突出特点是 CH2/CH3 和 C=O/C=C 的值相对较高,而 CHal/C=O 和 CC 的值明显较低。具体来说,卡林蝶叶轴角质层的 CHal/C=O 比值相对较低,这与现生叶片和化石叶片角质层的情况一致。较低的 CHal/C=O 比率表明,CO 基团在角质层和角质层中形成可变形的柔性结构方面可能发挥了重要作用。这种刚性的降低表明曾经生活过的卡林蝶植物的叶轴具有很高的柔韧性,从而支持了对攀援或藤本植物习性的解释。角质分离及其化学特性揭示了卡林蝶轴可能具有的生物力学(柔韧性)特性,从而加深了我们对植物生长习性的了解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Fossil cutin of Karinopteris (Middle Pennsylvanian pteridosperm) from the “paper” coal of Indiana, U.S.A.

Fossil cutin of Karinopteris (Middle Pennsylvanian pteridosperm) from the “paper” coal of Indiana, U.S.A.

Fossil cutin of Karinopteris (Middle Pennsylvanian pteridosperm) from the “paper” coal of Indiana, U.S.A.

For the first time, a cutin-like, highly chemically resistant macropolymer has been isolated from rachises of Karinopteris sp. (lyginopteridalean pteridosperm, Middle Pennsylvanian). Samples are obtained from a cuticular or “paper” coal-shale, i.e., an organic-rich and highly clastic rock associated with the Upper Block Coal Member of the Brazil Formation, Parke County, west-central Indiana, U.S.A. Karinopteris specimens are preserved as naturally oxidized compressions, termed “fossilized cuticles”, and possibly represent vegetation of mineral substrate environments. Employing laboratory oxidation reactions, the fossilized cuticle of Karinopteris rachises is used to obtain the cuticle. After additional and long-term oxidation treatment, the cuticle yields the cutin-like macropolymer, here referred to as “cutin” for simplicity. The fossilized cuticle, cuticle, and cutin samples of Karinopteris sp. are chemically analyzed using semi-quantitative Fourier transform infrared (FTIR) spectroscopy. Cutin IR spectra of Karinopteris rachises are characterized by (a) a predominantly aliphatic composition as indicated by intense aliphatic (CHal) CH stretching peaks at 3000–2700 cm−1, which are assigned to methylene (CH2) and methyl (CH3) groups; (b) carbonyl (C=O) groups at 1730–1640 cm−1, and aromatic carbon (C=C) absorption bands at 1600–1500 cm−1. A comparison with the cuticle, the cutin stands out due to relatively higher values of CH2/CH3 and C=O/C=C, while displaying notably low values of CHal/C=O and CC contribution. Specifically, the relatively low value of CHal/C=O ratio obtained for the cutin of Karinopteris rachises is consistent with those found in the cutin of extant and fossil leaves. This lower CHal/C=O ratio indicates the important role likely played by CO groups in creating a deformable and flexible structure in both the cutin and the cuticle. Such a reduced rigidity suggests a high level of rachis flexibility of the once-living Karinopteris plant, supporting the interpretation of a climbing or liana habit. Cutin isolation and its chemical characterization shed light on the probable biomechanical (flexibility) properties of Karinopteris rachises, thereby enhancing our understanding of the plant growth habit.

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来源期刊
International Journal of Coal Geology
International Journal of Coal Geology 工程技术-地球科学综合
CiteScore
11.00
自引率
14.30%
发文量
145
审稿时长
38 days
期刊介绍: The International Journal of Coal Geology deals with fundamental and applied aspects of the geology and petrology of coal, oil/gas source rocks and shale gas resources. The journal aims to advance the exploration, exploitation and utilization of these resources, and to stimulate environmental awareness as well as advancement of engineering for effective resource management.
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