Age Estimation using Phalangeal Skeletochronology in Northern Crawfish Frogs, Lithobates areolatus circulosus (Amphibia: Anura: Ranidae), from Arkansas

S. Trauth, C. Thigpen
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Abstract

As an obligate crayfish burrow dweller, crawfish frogs have historically occupied a relatively narrow ecological niche throughout their distribution in the tall grass prairies and grasslands of the central and southcentral United States (Redmer 2000; Powell et al. 2016; Lannoo et al. 2018). Habitat loss and shifting climate patterns pose as major threats to the continued existence of this species (Lannoo and Stiles 2017). In Arkansas, the Northern Crawfish Frog, Lithobates areolatus circulosus, occurs in only 19 of its 75 counties (Trauth et al. 2004; Trauth and Holt 2017). Because of their secretive nature, late winter-early spring breeding season, and current protected status by the Arkansas Game and Fish Commission, this species remains a rarity in most museum collections in the state (Trauth et al. 2004). Moreover, only anecdotal information exits regarding any aspect of their natural history in Arkansas (Trauth et al. 1990). In the present study, we chose to conduct a phalangeal skeletochronological investigation of the Northern Crawfish Frog utilizing museum specimens (n = 10) deposited in the herpetological collection (ASUMZ 13900, 14150, 31084-86, 33746-49, 33611) housed in the Arkansas Center for Biodiversity Collections located at Arkansas State University. Four frogs included in this sample were recently collected by SET while road cruising on Turkey Pond Loop (35.2147195N, 92.7567921W) in Conway County on the 20 and 27 February, 2018. Our goals were to estimate the age of individuals within this small Arkansas frog sample by counting annular lines of arrested growth (LAGs) and compare these results with the age estimates found for this frog by Redmer (2000), who utilized the same histological technique on a crawfish frog population in southern Illinois. The distal phalanx (Fig. 1) of the 4 toe of the left hind foot from each frog was removed and placed into either 70% ethanol (historic specimens) or 10% neutral buffered formalin for fresh toes. Then, we treated all toes with a decalcifying solution (1% hydrochloric acid) Figure 1. Photomicrograph of a transverse section through the distal phalanx of Lithobates areolatus circulosus (ASUMZ 33748) revealing phalangeal bone (Pb). Sm = striated muscle.
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阿肯色州北部小龙虾蛙石斑蛙(两栖纲:蛙科)的指骨骨骼年表年龄估计
作为一种义务性小龙虾穴居动物,小龙虾蛙在美国中部和中南部的高草草原和草原上的分布历来占据着相对狭窄的生态位(Redmer 2000;Powell等人2016;Lannoo等人2018)。栖息地的丧失和气候模式的变化对该物种的持续存在构成了主要威胁(Lannoo和Stiles,2017)。在阿肯色州,北方小龙虾蛙Lithobates areolatus circulous只出现在75个县中的19个县(Trauth等人,2004年;Trauth和Holt,2017年)。由于其隐秘的性质、冬末春初的繁殖季节以及目前受到阿肯色州狩猎和鱼类委员会的保护,该物种在该州大多数博物馆藏品中仍然是罕见的(Trauth等人,2004)。此外,只有关于他们在阿肯色州自然历史的任何方面的轶事信息存在(Trauth等人,1990)。在本研究中,我们选择利用位于阿肯色州立大学的阿肯色生物多样性收藏中心的爬行动物收藏馆(ASUMZ 139001415031084-863346-4933611)中存放的博物馆标本(n=10),对北方小龙虾蛙进行指骨骨骼年代调查。SET最近于2018年2月20日和27日在康威县的土耳其池塘环路(35.2147195N,92.7567921W)公路巡航时采集了该样本中的四只青蛙。我们的目标是通过计数生长停滞的环状线(LAG)来估计阿肯色州小青蛙样本中个体的年龄,并将这些结果与Redmer(2000)对这种青蛙的年龄估计进行比较,Redmer对伊利诺伊州南部的小龙虾蛙种群使用了相同的组织学技术。取下每只青蛙左后脚4趾的远端指骨(图1),并将其放入70%乙醇(历史标本)或10%中性缓冲福尔马林中,用于新鲜脚趾。然后,我们用脱钙溶液(1%盐酸)处理所有脚趾(图1)。圆形石斑藻(ASUMZ 33748)远端指骨的横截面显微照片,显示指骨(Pb)。Sm=横纹肌。
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