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首页> 外文期刊>Palaios: An International Journal of the Society of Economic Paleontologists & Mineralogists >Fish feeding traces from middle Eocene limestones (Gargano Promontory, Apulia, Southern Italy)
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Fish feeding traces from middle Eocene limestones (Gargano Promontory, Apulia, Southern Italy)

机译:来自始新世中期石灰岩的鱼类取食痕迹(意大利南部普利亚大区加尔加诺角)

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摘要

More than two hundred subcircular to crescent-shaped depressions, often with radiating markings, were discovered on a 120 m~2 bedding plane interpreted as base-of-slope carbonate deposits and belonging to the LutetianBartonian Peschici Formation at San Lorenzo (Vieste, Gargano Promontory, Italy). The area was mapped using a high-resolution aerial camera (mounted on a kite) and a terrestrial laser scanner. The survey allowed detailed morphologic analysis and topographic mapping of the traces, in order to analyze the very regular distribution pattern. The ichnological study, combined with sedimentologic and stratigraphic analyses, identifies the depressions as fish feeding traces. Although the tracemaker cannot be definitely identified, the comparison with modern and fossil fish excavations suggests a higher affinity with bony fishes (e.g., sturgeons) than with rays. The trace fossils are here attributed to the ichnogenus Piscichnus and constitute the first discovery of this ichnotaxon in the middle Eocene of the Apulia Carbonate Platform and of Italy.
机译:在一个120 m〜2的层理平面上发现了200多个亚圆形至新月形的凹陷,这些凹陷通常带有放射状标记,被解释为斜坡碳酸盐岩沉积物,属于圣洛伦佐(Vieste,Gargano Promontory , 意大利)。使用高分辨率的航拍相机(安装在风筝上)和地面激光扫描仪绘制了该区域的地图。该调查允许对痕迹进行详细的形态分析和地形图绘制,以便分析非常规则的分布模式。海洋学研究与沉积学和地层学分析相结合,将凹陷确定为鱼类的觅食痕迹。尽管无法确切地确定示踪者,但与现代和化石鱼发掘的比较表明,对骨鱼(例如st鱼)的亲和力高于对射线的亲和力。这里的痕迹化石归因于鱼鳞鱼类,是在普利亚碳酸盐岩台地和意大利的始新世中期发现的这种鱼鳞生物的第一个发现。

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