Christman Mary C, Doctor Daniel H, Niemiller Matthew L, Weary David J, Young John A, Zigler Kirk S, Culver David C
Departments of Biology and of Statistics, University of Florida, Gainesville, Florida, and MCC Statistical Consulting LLC, Gainesville, Florida, United States of America.
U. S. Geological Survey, Reston, Virginia, United States of America.
PLoS One. 2016 Aug 17;11(8):e0160408. doi: 10.1371/journal.pone.0160408. eCollection 2016.
One of the most challenging fauna to study in situ is the obligate cave fauna because of the difficulty of sampling. Cave-limited species display patchy and restricted distributions, but it is often unclear whether the observed distribution is a sampling artifact or a true restriction in range. Further, the drivers of the distribution could be local environmental conditions, such as cave humidity, or they could be associated with surface features that are surrogates for cave conditions. If surface features can be used to predict the distribution of important cave taxa, then conservation management is more easily obtained. We examined the hypothesis that the presence of major faunal groups of cave obligate species could be predicted based on features of the earth surface. Georeferenced records of cave obligate amphipods, crayfish, fish, isopods, beetles, millipedes, pseudoscorpions, spiders, and springtails within the area of Appalachian Landscape Conservation Cooperative in the eastern United States (Illinois to Virginia and New York to Alabama) were assigned to 20 x 20 km grid cells. Habitat suitability for these faunal groups was modeled using logistic regression with twenty predictor variables within each grid cell, such as percent karst, soil features, temperature, precipitation, and elevation. Models successfully predicted the presence of a group greater than 65% of the time (mean = 88%) for the presence of single grid cell endemics, and for all faunal groups except pseudoscorpions. The most common predictor variables were latitude, percent karst, and the standard deviation of the Topographic Position Index (TPI), a measure of landscape rugosity within each grid cell. The overall success of these models points to a number of important connections between the surface and cave environments, and some of these, especially soil features and topographic variability, suggest new research directions. These models should prove to be useful tools in predicting the presence of species in understudied areas.
由于采样困难,原地研究最具挑战性的动物群之一是专性洞穴动物群。洞穴受限物种分布零散且范围有限,但通常不清楚观察到的分布是采样假象还是真正的范围限制。此外,分布的驱动因素可能是当地环境条件,如洞穴湿度,也可能与作为洞穴条件替代指标的地表特征有关。如果地表特征可用于预测重要洞穴类群的分布,那么保护管理就更容易实现。我们检验了这样一个假设,即基于地表特征可以预测专性洞穴物种主要动物群的存在。美国东部阿巴拉契亚景观保护合作区内(从伊利诺伊州到弗吉尼亚州,从纽约州到阿拉巴马州)洞穴专性双足节肢动物、小龙虾、鱼类、等足类动物、甲虫、千足虫、伪蝎、蜘蛛和跳虫的地理参考记录被分配到20×20千米的网格单元中。使用逻辑回归模型,利用每个网格单元内的20个预测变量(如岩溶百分比、土壤特征、温度、降水量和海拔)对这些动物群的栖息地适宜性进行建模。对于单个网格单元特有物种的存在以及除伪蝎外的所有动物群,模型成功预测某一动物群存在的时间超过65%(平均为88%)。最常见的预测变量是纬度、岩溶百分比和地形位置指数(TPI)的标准差,TPI是衡量每个网格单元内景观粗糙度的指标。这些模型的总体成功表明地表环境和洞穴环境之间存在许多重要联系,其中一些联系,特别是土壤特征和地形变异性,为新的研究方向提供了思路。这些模型应被证明是预测未充分研究地区物种存在的有用工具。