白垩纪某些亚氨体缝合线长度与膈腔容积的异速测量

IF 1.3 4区 地球科学 Q3 PALEONTOLOGY Paleontological Research Pub Date : 2022-01-01 DOI:10.2517/PR200031
Haruna Furui, T. Ubukata
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引用次数: 0

摘要

摘要对日本北海道上白垩纪野佐群6种菊石属28个标本的缝合线长度与膈腔体积的异速关系进行了研究。缝合线周长是通过将照片中沿缝合线的数字化点之间的距离相加来计算的。使用改进的Raup模型计算膜腔体积。每个物种的缝合线周长和膈腔体积之间的关系表示为对数尺度上的异速方程。个体发育异速指数在0.462~0.626之间。估计的指数远大于等距情况下的指数(0.333)和之前通过种间比较获得的值。使用理论形态学模型的计算表明,缝线周长约为0.5的异速指数反映了间隔表面积相对于身体大小的正异速指数。目前的结果表明,缝合线周长的强阳性异径测量导致间隔表面积的相当大的正异径测量,从而满足Kleiber标度定律,尽管其功能意义尚不清楚。
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Allometry between Suture Line Length and Phragmocone Volume in Some Cretaceous Ammonoids
Abstract. The allometric relationship between suture line length and phragmocone volume was examined in 28 specimens belonging to six ammonoid species recovered from the Upper Cretaceous Yezo Group of Hokkaido, Japan. The suture perimeter was calculated by summing the distances between digitized points along the suture line in a photograph. The phragmocone volume was calculated using a modified Raup's model. The relationship between suture perimeter and phragmocone volume in each species was expressed as an allometric equation on a logarithmic scale. The exponent of ontogenetic allometry estimated for each species ranged from 0.462 to 0.626. The exponents estimated were much greater than the exponent in the case of isometry (0.333) and the value previously obtained through interspecific comparison. Calculation using a theoretical morphologic model indicates that allometric exponents for the suture perimeter of approximately 0.5 reflect positive allometry of the septal surface area with respect to body size. The present results suggest that strong positive allometry of the suture perimeter leads to a considerable positive allometry of the septal surface area resulting in satisfying Kleiber's scaling law, although its functional significance remains unclear.
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来源期刊
Paleontological Research
Paleontological Research PALEONTOLOGY-
CiteScore
1.60
自引率
0.00%
发文量
47
审稿时长
>12 weeks
期刊介绍: Paleonotological Research (PR) is a quarterly, peer-reviewed international journal, which focuses on original contributions primarily in the area of paleontology but also covering a wide range of allied sciences. It has been published since 1997 as a successor to the former journal Transactions and Proceedings of the Palaeontological Society of Japan. The emphasis of contributions will include global and local perspectives, and contents can cover all ages (Precambrian to the Quaternary, including the present time).
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