BITE MARKS ON A SKULL OF PSEUDOPALATUS MCCAULEYI (ARCHOSAURIA: CRUROTARSI: PHYTOSAURIDAE) FROM THE UPPER TRIASSIC BULL CANYON FORMATION, EASTERN NEW MEXICO

L. Rinehart, A. Heckert, S. Lucas, D. C. Bond
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引用次数: 2

Abstract

A 1.12 meter-long brachyrostral phytosaur skull (NMMNH P- 56187) from the Upper Triassic Bull Canyon Formation of eastern New Mexico is assigned to Pseudopalatus mccauleyi based on its poorly preserved, but apparently depressed supratemporal fenestrae, its subtriangular squamosal process, and completely crested rostrum. The skull is obliquely flattened, exposing the left side of the face and skull roof. The lachrymal - nasal area, bounded by the external nares, antorbital fenestra (aofe) and orbit, on the left side is punctured by three large holes, one immediately dorsal to the middle of the aofe and two more (paired?) posterior to the first and approximately halfway between the aofe and the orbit. Based on size and shape, these holes appear to represent bite marks, probably from another (possibly conspecific) phytosaur. The three marks thus form an “L” and probably represent two teeth from one side of the biting animal’s jaw and a one from the other, although the orientation of attack is not clear. The larger holes may mark wounds inflicted by the large teeth in the “bulb” of a phytosaur snout, with the smaller injury attributed to a smaller, more posterior tooth. The edges of the holes are smooth and rounded, evidently having healed. The tooth marks measure: (1) 27 X 10 mm, (2) 25 X 13 mm, and (3) 16 X14 mm. The combination of elongate and approximately round punctures supports assignment of the bite mark to the ichnotaxon Heterodontichnites hunti . This is only the second bite mark on a phytosaur fossil of which we are aware. The other is in the palate of a large skull of Redondasaurus bermani (NMMNH P-31094) from the Redonda Formation of east-central New Mexico. This injury comprises three smaller (9 to 12 mm), approximately round punctures in a gently curved line that is 45 mm long. These punctures show healed edges and may have been self-inflicted. Thus, the Pseudopalatus bite mark is the first unambiguous evidence of a phytosaur suffering an attack from another phytosaur of which we are aware.
新墨西哥东部上三叠世公牛峡谷地层出土的麦考利假腭龙颅骨上的咬痕(原龙目:棘龙目:植物龙科)
新墨西哥州东部上三叠统公牛峡谷组的一具1.12米长的短嘴植物龙头骨(NMMNH P- 56187),根据其保存较差但明显凹陷的颞上窗、近三角形的鳞状突起和完全有冠状突起的喙部,被认定为Pseudopalatus mccauleyi。头骨倾斜扁平,露出左脸和头骨顶部。泪腺-鼻区,以外鼻、眶前孔和眼眶为界,在左侧被三个大孔刺穿,一个紧靠眶前孔的中间,另外两个(成对)在第一个孔的后面,大约在眶前孔和眼眶的中间。根据大小和形状,这些洞似乎代表了咬痕,可能来自另一种(可能是同属的)植龙。这三个标记形成了一个“L”形,可能代表了咬人的动物下巴一侧的两颗牙齿和另一侧的一颗牙齿,尽管攻击的方向尚不清楚。较大的洞可能是植龙鼻子“球”上的大牙齿造成的伤口,较小的伤口是由更小、更靠后的牙齿造成的。洞口的边缘光滑圆润,显然已经愈合了。牙印尺寸:(1)27 × 10毫米,(2)25 × 13毫米,(3)16 × 14毫米。长形和近似圆形的刺痕的结合支持了将咬痕归属于异齿龙(Heterodontichnites hunti)。这是我们所知的植龙化石上的第二个咬痕。另一个是在新墨西哥州中东部Redonda组的一个大头骨的上颚(NMMNH P-31094)。这种损伤包括三个较小的(9至12毫米),大约圆形的45毫米长的弯曲线穿刺。这些伤口边缘愈合,可能是自己造成的。因此,假腭龙的咬痕是我们所知的植物龙遭受另一种植物龙攻击的第一个明确证据。
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