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Bird and Mammal Footprints From the Tertiary of Navarre (Western Pyrenees)

机译:纳瓦拉(西比利牛斯山脉)第三纪的鸟类和哺乳动物的足迹

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A rich variety of vertebrate footprints is known from a number of Upper Eocene to Lower Miocene localities of Navarre (western Pyrenees). The sediments were deposited in a wide range of depositional environments, from marginal marine to diversified terrestrial. Abundant bird tracks have been found in the coastal deposits of the Upper Eocene Liedena Sandstone of the Yesa and Itzagaondoa areas. Ciconiiformes-like (Leptoptilostipus pyrenaicus) and Charadriiformes-like (Charadriipeda ichnospp.) footprints have been recognized. Mammal ichnites have been discovered in the Oligocene and Lower Miocene deposits of Navarre. Equoid perissodactyl ichnites similar to those of Plagiolophustipus occur in the Oligocene fluviatile rocks of the Mués Sandstone of Olexoa and the Rocaforte Sandstone near Oibar and Sada. Trackways of entelodontids (Entelodontipus) are known in fluviatile-palustrine beds of the Oligocene Mués Sandstone of Olkotz. Additionally, bird (Charadriiformes-like) tracks are known in fluviatile-palustrine floodplain deposits of the Lower Miocene Ujué Formation of Los Arcos. In the same area, the Desoio and Los Arcos outcrops have also yielded perissodactyl trackways of possible Equoidea. Trackways of rhinocerotids (?) and artiodactyls (possibly Pecoripeda) are described from the Lower Miocene (Ramblian) palustrine limestones marginal to the Lerín Formation of Kaparroso and from alluvial fan deposits of the Uncastillo-Perdón Formation of Altzorritz, respectively.
机译:从Navarre(西比利牛斯山脉)的上始新世到中新世的许多地方,已知有各种各样的脊椎动物足迹。沉积物沉积在从边缘海洋到多样化陆地的广泛沉积环境中。在Yesa和Itzagaondoa地区的上始新世Liedena砂岩海岸沉积物中发现了大量鸟类。已经认识到类似Ciconiiformes(Leptoptilostipus pyrenaicus)和类似Charadriiformes(Charadriipeda ichnospp。)的足迹。在纳瓦拉的渐新世和下中新世矿床中发现了哺乳动物的鱼类。类似于Plagiolophustipus的Equoid变色龙眼蛇纹石出现在Olexoa的Mués砂岩和Oibar和Sada附近的Rocaforte砂岩的渐新世易碎岩中。在奥尔科兹的渐新世Mués砂岩的通流-palustrine层中,已知牙齿石(Entelodontipus)的走道。此外,在洛斯阿尔科斯下中新世Ujué组的河流-河床-泛滥平原沉积物中还发现了鸟类(类Charadriiformes)的踪迹。在同一地区,Desoio和Los Arcos的露头也产生了可能的Equoidea的过月桂基径迹。犀角龙(?)和偶蹄动物(可能是Pecoripeda)的走道分别描述于卡帕罗索(Kaparroso)的莱林组边缘的下中新世(Ramblian)palustrine石灰石和阿尔索里茨的Uncastillo-Perdón组的冲积扇沉积物中。

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