La Sorte Frank A, Thompson Frank R
Department of Fisheries and Wildlife Sciences, University of Missouri, Columbia, Missouri 65211, USA.
Ecology. 2007 Jul;88(7):1803-12. doi: 10.1890/06-1072.1.
Climate change is thought to promote the poleward movement of geographic ranges; however, the spatial dynamics, mechanisms, and regional anthropogenic drivers associated with these trends have not been fully explored. We estimated changes in latitude of northern range boundaries, center of occurrence, and center of abundance for 254 species of winter avifauna in North America from 1975 to 2004. After accounting for the effect of range size and the location of the northern boundary, positive latitudinal trends were evident for the northern boundary (1.48 km/yr), center of occurrence (0.45 km/yr), and center of abundance (1.03 km/yr). The northern boundary, when examined across individual species, had the most variable trends (SD = 7.46 km/yr) relative to the center of occurrence (SD = 2.36 km/yr) and center of abundance (SD = 5.57 km/yr). Trends did not differ based on migratory status, but there was evidence that trends differed for species with ranges centered in the southern vs. northern portion of the study area. Species occurred more sporadically over time at northern range boundaries, and northern boundaries were associated with a concentration of colonization and extirpation events, with a greater prevalence of colonization events likely promoting poleward trends. Regional anthropogenic drivers explained approximately 8% of the trend for the northern boundary, 14% for the center of occurrence, and 18% for the center of abundance; however, these effects were localized in the northern portion of species' ranges and were associated with distributional changes within ranges, primarily abundance, producing patterns that mimicked poleward movements. We conclude that poleward distributional shifts represent the interaction between climate change and regional factors whose outcome is determined by the scale of the analysis and the biotic and abiotic features in the region, and how anthropogenic activities have impacted these features.
气候变化被认为会促使地理分布范围向极地移动;然而,与这些趋势相关的空间动态、机制以及区域人为驱动因素尚未得到充分探究。我们估算了1975年至2004年间北美254种冬季鸟类的北部分布范围边界、出现中心和丰富度中心的纬度变化。在考虑了分布范围大小和北部分布边界位置的影响后,北部分布边界(1.48千米/年)、出现中心(0.45千米/年)和丰富度中心(1.03千米/年)呈现出明显的正向纬度趋势。相对于出现中心(标准差 = 2.36千米/年)和丰富度中心(标准差 = 5.57千米/年),北部分布边界在单个物种层面上的趋势变化最大(标准差 = 7.46千米/年)。趋势不因迁徙状态而有所不同,但有证据表明,分布范围集中在研究区域南部与北部的物种,其趋势存在差异。随着时间推移,物种在北部分布边界的出现更为零散,并且北部分布边界与定殖和灭绝事件的集中发生相关,定殖事件的更普遍发生可能推动了向极地的趋势。区域人为驱动因素对北部分布边界趋势的解释约为8%,对出现中心趋势的解释约为14%,对丰富度中心趋势的解释约为18%;然而,这些影响局限于物种分布范围的北部,并且与分布范围内的分布变化相关,主要是丰富度变化,产生了类似向极地移动的模式。我们得出结论,向极地的分布变化代表了气候变化与区域因素之间的相互作用,其结果取决于分析的尺度以及该区域的生物和非生物特征,以及人为活动如何影响了这些特征。