Suarez-Gonzalez Adriana, Sutton Jolene T, Trant Andrew J, Zamlynny Elena, Good Sara V
Department of Biology, The University of Winnipeg, 599 Portage Avenue, Winnipeg, Manitoba, R3B 2G3, Canada Department of Botany, University of British Columbia, 3529-6270 University Blvd., Vancouver, British Columbia, V6T 1Z4, Canada.
Department of Biology, University of Hawai'i at Mānoa, 2538 McCarthy Mall, Honolulu, Hawaii 96822 USA Department of Biology, Acadia University, 33 Westwood Avenue, Wolfville, Nova Scotia, B4P 2R6, Canada.
Am J Bot. 2015 Apr;102(4):609-20. doi: 10.3732/ajb.1400254. Epub 2015 Apr 6.
Molecular population genetics is a powerful tool to infer how species responded to past environmental change. In the northern hemisphere, interest is increasing in how species responded to changes in ice coverage and temperature during the last glaciation maximum (LGM, between 18000-21000 yr ago) with a common assumption that glacial refugia were located at the southern edge of a species range.
We reconstructed the glacial and postglacial phylogeography of Sabatia kennedyana, a member of the Atlantic Coastal Plains Flora with a current distribution from Nova Scotia (NS) to South Carolina, using both cpDNA and nuclear markers. We also examined clinal variation in morphological traits, in particular relative investment in asexual vs sexual growth.
We find strong evidence that the species did not reside in southern glacial refugia, but rather in primary glacial refugia off the exposed continental shelf extending from Cape Cod and that this area was responsible for the founding of modern populations across the range from Nova Scotia (NS) to the United States. Additionally, based on the finding of higher cpDNA diversity and older cpDNA lineages in NS, we propose that multiple founder events occurred in NS, while only a single lineage gave rise to current populations in the United States.
By understanding how S. kennedyana responded to past shifts in climate and by identifying areas of high genetic diversity in the northern range edge, we discuss the potential response of the species to future climate change scenarios.
分子群体遗传学是推断物种如何应对过去环境变化的有力工具。在北半球,人们越来越关注物种在末次盛冰期(LGM,距今18000 - 21000年前)期间如何应对冰盖和温度变化,普遍认为冰期避难所位于物种分布范围的南缘。
我们利用叶绿体DNA(cpDNA)和核标记,重建了肯尼迪半边莲(Sabatia kennedyana)的冰期和冰后期系统地理学,该植物是大西洋沿岸平原植物区系的成员,目前分布于新斯科舍省(NS)至南卡罗来纳州。我们还研究了形态特征的渐变变异,特别是无性与有性生长的相对投入。
我们发现有力证据表明,该物种并非栖息于南部冰期避难所,而是位于从科德角延伸出的裸露大陆架外的主要冰期避难所,并且该区域是从新斯科舍省(NS)到美国整个分布范围内现代种群的起源地。此外,基于在新斯科舍省发现的更高的cpDNA多样性和更古老的cpDNA谱系,我们提出在新斯科舍省发生了多次奠基者事件,而在美国只有一个谱系产生了当前的种群。
通过了解肯尼迪半边莲如何应对过去的气候变化,并确定其北部分布边缘的高遗传多样性区域,我们讨论了该物种对未来气候变化情景的潜在响应。