科罗拉多东南部发现的霸王龙的证据

Q4 Earth and Planetary Sciences New Mexico Geology Pub Date : 2008-01-01 DOI:10.58799/nmg-v30n1.12
G. Osborn, K. Berry
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Theropod bones commonly exhibit onion-skin layering in cross section (K. Carpenter, pers. comm. 2007), and this bone seems to lack this feature, although the bone has distinct, differentiable layers. Whereas the bone itself may not be exclusively attributed to a theropod based on its gross histological properties alone, there are quantitative reasons supporting this diagnosis. First, the bone fragment is circular in cross section, and intersecting perpendicular bisectors of lines secant to its intact, periosteal surface suggest a radius of 90 ± 0.1 mm. As long bone circumference is used to estimate a live animal’s weight (Anderson et al. 1985; Alexander 1989), a 90 mm radius corresponds to a biped weighing approximately 5.23 metric tons. In Maastrichtian time in western North America, this value is exclusive to T. rex as far as mass estimates based on long bone circumferences for bipeds are concerned (Alexander 1989; Horner et al. 2004). Second, as T. rex femora have circular cross sections at their midpoint (Farlow et al. 1995; Holtz 2004) and the published growth curve for T. rex is based on midshaft femoral measurements (Erickson et al. 2004), it is possible to quantitatively compare the published growth curve for T. rex with the growth pattern observed in this specimen. Measuring the midpoint of each growth line to an accuracy of ± 0.5 mm along a radial transect, T. rex annual growth markers are exceptionally good predictors for the growth lines observed in this bone (cχ2 = 1.44, df = 6, p-value > 0.95). As T. rex is the only animal known to exhibit this characteristic pattern of growth (Erickson et al. 2004; ChinsamyTuran 2005), this is believed to be a fairly powerful diagnostic test. Significance—Estimated to be about 71 m.y. old based on the age of the Baculites eliasi ammonite zone, these fossils may be among the oldest known T. rex fossils (D. Wolberg, pers. comm. 2007). 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引用次数: 0

摘要

暴龙目奥斯本霸王龙科奥斯本1905属奥斯本暴龙1905 cf. T. rex Osborn 1905参考标本- tsjc 2008.1.1;TSJC 2008.1.2;TSJC 2008.1.3。描述-牙齿:根据牙冠形状和锯齿密度(N. Larson, pers.),一颗暴龙的牙齿(TSJC 2008.1.1)与“矮暴龙lancensis”(或幼年霸王龙,Carr and Williamson 2004)的牙齿最相似。通讯,2007)。在直线测量中,牙齿从尖端到基部约为3.5厘米。沿前隆突的锯齿密度为12个/厘米,证明诊断为霸王龙(Farlow et al. 1991)。牙齿稍弯曲,钝,沿其前隆突有小齿,在其基部断裂。股骨:一块肢骨碎片(TSJC 2008.1.2)也被初步鉴定为cf. T. rex。兽脚亚目恐龙的骨头在横截面上通常表现出洋葱皮的分层(K. Carpenter, pers。Comm . 2007),而这块骨头似乎缺乏这种特征,尽管骨头有明显的、可分化的层。然而,仅根据其大体组织学特征,骨骼本身可能不完全属于兽脚亚目恐龙,但有定量的原因支持这种诊断。首先,骨碎片的横截面呈圆形,与完整骨膜表面割线相交的垂直平分线显示其半径为90±0.1 mm。由于长骨周长被用来估计活体动物的体重(Anderson et al. 1985;Alexander 1989),一个90毫米的半径对应于一个重约5.23公吨的两足动物。在北美西部的马斯特里赫特时期,根据两足动物的长骨周长来估计质量,这个值是霸王龙所独有的(Alexander 1989;Horner et al. 2004)。其次,由于霸王龙股骨的中点截面呈圆形(Farlow et al. 1995;Holtz 2004)和已发表的暴龙生长曲线是基于股骨中轴测量(Erickson et al. 2004),因此可以将已发表的暴龙生长曲线与本标本中观察到的生长模式进行定量比较。测量每条生长线的中点沿径向样带的精度为±0.5 mm,霸王龙的年生长标记是该骨骼中观察到的生长线的非常好的预测因子(cχ2 = 1.44, df = 6, p值> 0.95)。由于霸王龙是已知唯一具有这种生长特征的动物(Erickson et al. 2004;ChinsamyTuran 2005),这被认为是一个相当强大的诊断测试。意义:根据埃利亚斯螺石带的年代估计,这些化石大约有71万年的历史,可能是已知最古老的霸王龙化石之一(D. Wolberg, pers。通讯,2007)。机构缩写- tsjc,特立尼达州立初级学院劳登-亨里茨考古博物馆。
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Evidence for a Tyrannosaurus rex from southeastern Colorado
Order SauriSchia Seeley 1888 Family TyrannoSauridae Osborn 1905 Genus Tyrannosaurus Osborn 1905 cf. T. rex Osborn 1905 Referred specimens—TSJC 2008.1.1; TSJC 2008.1.2; TSJC 2008.1.3. Description—Tooth: A tyrannosaurid tooth (TSJC 2008.1.1) most closely resembles the teeth of “Nanotyrannus lancensis” (or adolescent T. rex, Carr and Williamson 2004) based on crown shape and serration density (N. Larson, pers. comm. 2007). In straight-line measurement, the tooth is approximately 3.5 cm from tip to base. The serration density along the anterior carina is 12/cm, justifying the diagnosis as T. rex (Farlow et al. 1991). The tooth is slightly recurved, blunt, bears denticles along its anterior carina, and is broken at its base. Femur: A limb bone fragment (TSJC 2008.1.2) is also tentatively identified as cf. T. rex. Theropod bones commonly exhibit onion-skin layering in cross section (K. Carpenter, pers. comm. 2007), and this bone seems to lack this feature, although the bone has distinct, differentiable layers. Whereas the bone itself may not be exclusively attributed to a theropod based on its gross histological properties alone, there are quantitative reasons supporting this diagnosis. First, the bone fragment is circular in cross section, and intersecting perpendicular bisectors of lines secant to its intact, periosteal surface suggest a radius of 90 ± 0.1 mm. As long bone circumference is used to estimate a live animal’s weight (Anderson et al. 1985; Alexander 1989), a 90 mm radius corresponds to a biped weighing approximately 5.23 metric tons. In Maastrichtian time in western North America, this value is exclusive to T. rex as far as mass estimates based on long bone circumferences for bipeds are concerned (Alexander 1989; Horner et al. 2004). Second, as T. rex femora have circular cross sections at their midpoint (Farlow et al. 1995; Holtz 2004) and the published growth curve for T. rex is based on midshaft femoral measurements (Erickson et al. 2004), it is possible to quantitatively compare the published growth curve for T. rex with the growth pattern observed in this specimen. Measuring the midpoint of each growth line to an accuracy of ± 0.5 mm along a radial transect, T. rex annual growth markers are exceptionally good predictors for the growth lines observed in this bone (cχ2 = 1.44, df = 6, p-value > 0.95). As T. rex is the only animal known to exhibit this characteristic pattern of growth (Erickson et al. 2004; ChinsamyTuran 2005), this is believed to be a fairly powerful diagnostic test. Significance—Estimated to be about 71 m.y. old based on the age of the Baculites eliasi ammonite zone, these fossils may be among the oldest known T. rex fossils (D. Wolberg, pers. comm. 2007). Institutional abbreviation—TSJC, Trinidad State Junior College Louden-Henritze Archeology Museum.
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来源期刊
New Mexico Geology
New Mexico Geology Earth and Planetary Sciences-Geology
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期刊介绍: New Mexico Geology is a quarterly, peer-reviewed journal available by subscription. Articles of original research are generally less than 10,000 words in length and pertain to the geology of New Mexico and neighboring states, primarily for an audience of professional geologists or those with an interest in the geologic story behind the landscape. The journal also publishes abstracts from regional meetings, theses, and dissertations (NM schools), descriptions of new publications, book reviews, and upcoming meetings. Research papers, short articles, and abstracts from selected back issues of New Mexico Geology are now available as free downloads in PDF format. Back issues are also available in hard copy for a nominal fee.
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