Wilga CD, Lauder GV
Department of Ecology and Evolutionary Biology, University of California, Irvine, CA 92697, USA.
J Exp Biol. 1999;202(Pt 18):2413-2432. doi: 10.1242/jeb.202.18.2413.
Pectoral fins are one of the major features of locomotor design in ray-finned fishes and exhibit a well-documented phylogenetic transition from basal to derived clades. In percomorph fishes, the pectoral fins are often used to generate propulsive force via oscillatory movements, and pectoral fin propulsion in this relatively derived clade has been analyzed extensively. However, in the plesiomorphic pectoral fin condition, exemplified by sturgeon, pectoral fins extend laterally from the body in a generally horizontal orientation, have been assumed to generate lift to balance lift forces and moments produced by the heterocercal tail, and are not oscillated to generate propulsive force. The proposal that pectoral fins in fishes such as sturgeon generate lift during horizontal locomotion has never been tested experimentally in freely swimming fishes. In this paper, we examine the function of pectoral fins in sturgeon swimming at speeds from 0.5-3.0 L s(-)(1), where L is total body length. Sturgeon were studied during steady horizontal locomotion as well as while sinking and rising in the water column. Pectoral fin function was quantified using three-dimensional kinematics to measure the orientation of the fin surface, digital particle image velocimetry (DPIV) was used to describe flow in the wake of the fin and to estimate force exerted on the water, and electromyography was used to assess pectoral fin muscle function. Sturgeon (size range 25-32 cm total length) swam horizontally using continuous undulations of the body with a positive body angle that decreased from a mean of 20 degrees at 0.5 L s(-)(1) to 0 degrees at 3.0 L s(-)(1). Both the angle of the body and the pectoral fin surface angle changed significantly when sturgeon moved vertically in the water column. Three-dimensional kinematic analysis showed that during steady horizontal swimming the pectoral fins are oriented with a negative angle of attack predicted to generate no significant lift. This result was confirmed by DPIV analysis of the pectoral fin wake, which only revealed fin vortices, and hence force generation, during maneuvering. The orientation of the pectoral fins estimated by a two-dimensional analysis alone is greatly in error and may have contributed to previous suggestions that the pectoral fins are oriented to generate lift. Combined electromyographic and kinematic data showed that the posterior half of the pectoral fin is actively moved as a flap to reorient the head and body to initiate rising and sinking movements. A new force balance for swimming sturgeon is proposed for steady swimming and vertical maneuvering. During steady locomotion, the pectoral fins generate no lift and the positive body angle to the flow is used both to generate lift and to balance moments around the center of mass. To initiate rising or sinking, the posterior portion of the pectoral fins is actively moved ventrally or dorsally, respectively, initiating a starting vortex that, in turn, induces a pitching moment reorienting the body in the flow. Adjustments to body angle initiated by the pectoral fins serve as the primary means by which moments are balanced.
胸鳍是硬骨鱼运动设计的主要特征之一,并且呈现出从基部类群到衍生类群的系统发育转变,这一点已有充分记录。在鲈形目鱼类中,胸鳍常通过摆动运动来产生推进力,并且在这个相对衍生的类群中,胸鳍推进已经得到了广泛分析。然而,在以鲟鱼为代表的原始胸鳍形态中,胸鳍从身体向侧面水平延伸,一直被认为是产生升力以平衡歪尾产生的升力和力矩,并且不会摆动来产生推进力。关于鲟鱼等鱼类的胸鳍在水平游动时产生升力的说法,从未在自由游动的鱼类中进行过实验验证。在本文中,我们研究了鲟鱼在速度为0.5 - 3.0 L s⁻¹(L为全长)时胸鳍的功能。研究了鲟鱼在稳定水平游动以及在水柱中下沉和上升时的情况。使用三维运动学来测量鳍表面的方向,从而对胸鳍功能进行量化,利用数字粒子图像测速技术(DPIV)来描述鳍后方的水流并估计作用在水上的力,同时使用肌电图来评估胸鳍肌肉功能。全长范围为25 - 32厘米的鲟鱼通过身体的连续波动进行水平游动,身体呈正角度,该角度从0.5 L s⁻¹时的平均20度减小到3.0 L s⁻¹时的0度。当鲟鱼在水柱中垂直移动时,身体角度和胸鳍表面角度都会发生显著变化。三维运动学分析表明,在稳定水平游动期间,胸鳍以负攻角定向,预计不会产生显著升力。胸鳍尾流的DPIV分析证实了这一结果,该分析仅在机动过程中揭示了鳍涡旋以及由此产生的力。仅通过二维分析估计的胸鳍方向存在很大误差,这可能导致了之前认为胸鳍定向是为了产生升力的观点。肌电图和运动学数据相结合表明,胸鳍后半部分作为襟翼主动移动,以重新定向头部和身体,从而启动上升和下沉运动。针对稳定游动和垂直机动,提出了一种新的鲟鱼游动的力平衡模型。在稳定游动期间,胸鳍不产生升力,身体相对于水流的正角度既用于产生升力,也用于平衡围绕质心的力矩。为了启动上升或下沉,胸鳍后部分别主动向下或向上移动,引发一个起始涡旋,进而诱导一个俯仰力矩,使身体在水流中重新定向。胸鳍引发的身体角度调整是平衡力矩的主要方式。