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Stomping Around the Sump: Miocene Pygmy Gomphothere from Esmeralda County, Nevada

机译:围绕底花踩下:内华达州Esmeralda County的Miocene Pygmy Gomphothere

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Here we describe an individual gomphothere specimen recovered from Esmeralda County, Nevada. It was recovered from an area known as "The Sump," just 18 miles north of Dyer, NV, currently dominated by badland topography. Remnants of a paleo-forest are visible in the highlands of the site, while the central basin exposes mudrocks and sandstones, interfingered in places by several chalky, volcaniclastic layers. The sediments denote a past marsh environment, an ideal feeding ground for browsers of C_3 plant material, such as trees and shrubs. A slot canyon feeds the inactive channel where the discovery was made. Sedimentary units of the Esmeralda Formation in the vicinity of the north end of Fish Lake Valley have previously been interpreted as Miocene (Claredonian North American Land Mammal Age). The Gomphotheriidae were a family of proboscideans, widespread throughout the late Cenozoic era. Gomphotheres radiated throughout North America during the Miocene epoch, and diversified throughout the continent until their extinction in the late Pleistocene. Several species were participants in the Great American Biotic Interchange, but only three have been recorded from South America. Gomphotheres likely filled the niche of a dominant megafaunal browser, as their dentition and body morphology suggest that they were opportunistic feeders with a preference for C3 browse. The recovered specimen represents the maxillae, portions of the premaxillae, as well as the palatine, all in articulation. After removal of sediment with an air scribe, anterior and posterior sinus cavities were revealed. Two molars are present, and a portion of both tusks have been preserved within their cranial sockets. We attribute this specimen to Gomphotherium minor based upon the combination of small potential skull size with the extremely worn occlusal surface of the preserved molars of the individual. Modern elephants exhibit similar tooth wear towards the end of their lives, eventually succumbing to starvation. Mawby (1968) described Megabelodon minor (later synonymized with Gomphotherium by Tobien 1973) based on a tuskless mandible recovered from the same formation. Diagnostic measurements of the teeth, maxillae, and palate were taken and compared to the type specimen and other longirostrine proboscideans. We believe that the individual collected from the Sump is of the same species, but this is difficult to confirm due to our lack of a dentary present.
机译:在这里,我们描述了从内华达州Esmeralda县回收的个体卤素标本。它是从被称为“贮槽”的区域中恢复过,NV北部仅18英里,目前由荒地地形主导。古林的残余在现场的高地可见,而中央盆地暴露泥质和砂岩,在几个白垩,火山的山上的地方接触。沉积物表示过去的沼泽环境,是C_3植物材料的浏览器的理想喂养地,如树木和灌木。插槽峡谷馈送发现发现的非活动通道。 Fish Lake Valley北端附近的Esmeralda形成的沉积单位以前被解释为内科(克拉登尼亚北美哺乳动物年龄)。 Gomphotheriidae是一系列经验丰富的家庭,在整个新生代时代普遍存在。在内科时代的北美辐射的植物辐射,并在整个大陆中多元化,直到它们在晚熟中的灭绝。几种物种是伟大的美国生物交换的参与者,但只有三个已从南美记录。 Gomphotheres可能填充了一个主要的Megafaunal浏览器的利基,因为他们的牙齿和身体形态表明他们是机会主义的饲养者,优先考虑C3浏览。回收的样本代表着颌骨部分,以及腭,均在关节中。用空气划线除去沉淀物后,揭示了前颌窦腔。存在两磨牙,并且在其颅骨插座中保存了两种牙科料。基于小潜在颅骨尺寸的组合,将该样品归因于基于小型潜在颅骨尺寸的组合,具有极其磨损的臼齿的个体的胶凝表面。现代大象在他们的生活结束时表现出类似的牙齿磨损,最终屈服于饥饿。 MAWBY(1968)基于从同一地层恢复的螺旋下颌骨,描述了MEGABELODON MENSED(稍后与TOBIEN 1973同义)。采集牙齿,上颌和腭的诊断测量,并与样品和其他长鼻葡萄酒验起的牙齿相比。我们认为,从贮槽中收集的个体是相同的物种,但由于我们缺乏伪心存在,这很难确认。

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