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从密集堆积的中新世贝壳层中自动确定化石牡蛎壳的三维方向。

Automatic determination of 3D orientations of fossilized oyster shells from a densely packed Miocene shell bed.

作者信息

Puttonen Ana, Harzhauser Mathias, Puttonen Eetu, Mandic Oleg, Székely Balázs, Molnár Gábor, Pfeifer Norbert

机构信息

1Department of Geodesy and Geoinformation, Vienna University of Technology, Vienna, Austria.

2Geological Paleontological Department, Natural History Museum Vienna, Vienna, Austria.

出版信息

Int J Earth Sci. 2018;107(6):2125-2142. doi: 10.1007/s00531-018-1591-0. Epub 2018 Feb 23.

Abstract

Shell beds represent a useful source of information on various physical processes that cause the depositional condition. We present an automated method to calculate the 3D orientations of a large number of elongate and platy objects (fossilized oyster shells) on a sedimentary bedding plane, developed to support the interpretation of possible depositional patterns, imbrications, or impact of local faults. The study focusses on more than 1900 fossil oyster shells exposed in a densely packed Miocene shell bed. 3D data were acquired by terrestrial laser scanning on an area of 459 m with a resolution of 1 mm. Bivalve shells were manually defined as 3D-point clouds of a digital surface model and stored in an ArcGIS database. An individual shell coordinate system (ISCS) was virtually embedded into each shell and its orientation was determined relative to the coordinate system of the entire, tectonically tilted shell bed. Orientation is described by the rotation angles roll, pitch, and yaw in a Cartesian coordinate system. This method allows an efficient measurement and analysis of the orientation of thousands of specimens and is a major advantage compared to the traditional 2D approach, which measures only the azimuth (yaw) angles. The resulting data can variously be utilized for taphonomic analyses and the reconstruction of prevailing hydrodynamic regimes and depositional environments. For the first time, the influence of possible post-sedimentary vertical displacements can be quantified with high accuracy. Here, the effect of nearby fault lines-present in the reef-was tested on strongly tilted oyster shells, but it was found out that the fault lines did not have a statistically significant effect on the large tilt angles. Aside from the high reproducibility, a further advantage of the method is its non-destructive nature, which is especially suitable for geoparks and protected sites such as the studied shell bed.

摘要

贝壳层是有关导致沉积条件的各种物理过程的有用信息来源。我们提出了一种自动化方法,用于计算沉积层面上大量细长和扁平物体(化石牡蛎壳)的三维方向,该方法的开发是为了支持对可能的沉积模式、叠瓦状结构或局部断层影响的解释。该研究聚焦于中新世一个密集堆积的贝壳层中暴露的1900多个化石牡蛎壳。通过地面激光扫描在面积为459平方米、分辨率为1毫米的区域获取三维数据。双壳类贝壳被手动定义为数字表面模型的三维点云,并存储在ArcGIS数据库中。一个单独的贝壳坐标系(ISCS)被虚拟地嵌入到每个贝壳中,其方向相对于整个构造倾斜贝壳层的坐标系确定。方向在笛卡尔坐标系中由滚动角、俯仰角和偏航角描述。这种方法允许对数千个标本的方向进行高效测量和分析,与仅测量方位角(偏航角)的传统二维方法相比,这是一个主要优势。所得数据可用于多种埋藏学分析以及对主要水动力状态和沉积环境的重建。首次能够高精度地量化可能的沉积后垂直位移的影响。在这里,对礁体中存在的附近断层线对强烈倾斜的牡蛎壳的影响进行了测试,但发现断层线对大倾斜角没有统计学上的显著影响。除了高再现性外,该方法的另一个优点是其非破坏性,这特别适用于地质公园和受保护地点,如所研究的贝壳层。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7e1e/6096536/49623261ff90/531_2018_1591_Fig1_HTML.jpg

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