沉积岩芯的高分辨率三维图像是探索有孔虫微生境的有力工具

IF 1.5 4区 地球科学 Q2 PALEONTOLOGY
M.P. Nardelli , N. Vanderesse , M. Moller , C. Guilhermic , A. Mouret
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引用次数: 0

摘要

底栖有孔虫是海洋原生动物,主要用作古环境的生物指标和代用指标。上底栖生物生活在沉积物表面或沉积物表面以上,因此被用作底层水条件的代用指标,而下底栖生物则生活在沉积物柱体中,因此可追踪孔隙水的化学性质。在本研究中,我们对一个实验性沉积物岩芯进行了显微层析成像分析,以观察两种表栖有孔虫 Ammonia confertitesta 和 Haynesina germanica 的生活位置。我们获得的图像首次提供了在三维空间中以 13 μm/voxel 的数值分辨率观察每个个体的可能性。结果表明,这两个物种从不位于沉积物表面以上或沉积物表面,而是在表层以下 0-500 μm 范围内的次表层沉积层中拥有其偏好的微生境。对沉积物岩心进行μCT扫描也是获得有孔虫生态学高分辨率信息的重要工具。所述方法有助于评估所有有孔虫物种的有效微生境,这些物种通常被用作古记录的代用指标,以确保我们从它们身上获得的信息可归因于特定沉积深度的底层水或孔隙水条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

High resolution 3D images of sediment cores as powerful tool for exploring foraminiferal microhabitats

High resolution 3D images of sediment cores as powerful tool for exploring foraminiferal microhabitats

Benthic foraminifera are marine protists largely used as bioindicators and proxies of paleo- environments. Epifaunal species are supposed to live at or above the sediment surface and are therefore used as proxies for bottom water conditions, while infaunal inhabit the sediment column, thus tracing porewater chemistry. Traditional analytical methods based on core slicing, however, have a low resolution that does not allow to precisely characterise the preferential microhabitat(s) of indicator species.

In this study we performed microtomographic analyses on an experimental sediment core, to observe the life-position of living foraminifera of two surface-dwelling species Ammonia confertitesta and Haynesina germanica, reported both as epifaunal or shallow infaunal. The images we obtained offered for the first time the possibility to observe each individual in 3D space with a numerical resolution of 13 μm/voxel.

The results revealed that the two species are never located above or at the sediment surface and have their preferential microhabitats in a sub-superficial sediment layer constrained in the 0–500 μm interval below the surface. Rapid decrease of abundances below this layer suggests that their microhabitat could be even more specific than previously thought.

μCT-scan of sediment cores is also a valuable tool to obtain high-resolution information about foraminiferal ecology. The described method is useful to assess the effective microhabitat of all foraminiferal species that are usually used as proxies for paleorecords, to ensure that the information we can obtain from them is attributable to bottom water or to porewater conditions at a specific sediment depth.

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来源期刊
Marine Micropaleontology
Marine Micropaleontology 地学-古生物学
CiteScore
3.70
自引率
15.80%
发文量
62
审稿时长
26.7 weeks
期刊介绍: Marine Micropaleontology is an international journal publishing original, innovative and significant scientific papers in all fields related to marine microfossils, including ecology and paleoecology, biology and paleobiology, paleoceanography and paleoclimatology, environmental monitoring, taphonomy, evolution and molecular phylogeny. The journal strongly encourages the publication of articles in which marine microfossils and/or their chemical composition are used to solve fundamental geological, environmental and biological problems. However, it does not publish purely stratigraphic or taxonomic papers. In Marine Micropaleontology, a special section is dedicated to short papers on new methods and protocols using marine microfossils. We solicit special issues on hot topics in marine micropaleontology and review articles on timely subjects.
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