CCMAR - CIMAR Laboratório Associado, Universidade do Algarve - Campus de Gambelas, Faro, 8005-139 Portugal.
BMC Biol. 2013 Jan 23;11:6. doi: 10.1186/1741-7007-11-6.
Significant effects of recent global climate change have already been observed in a variety of ecosystems, with evidence for shifts in species ranges, but rarely have such consequences been related to the changes in the species genetic pool. The stretch of Atlantic coast between North Africa and North Iberia is ideal for studying the relationship between species distribution and climate change as it includes the distributional limits of a considerable number of both cold- and warm-water species.We compared temporal changes in distribution of the canopy-forming alga Fucus vesiculosus with historical sea surface temperature (SST) patterns to draw links between range shifts and contemporary climate change. Moreover, we genetically characterized with microsatellite markers previously sampled extinct and extant populations in order to estimate resulting cryptic genetic erosion.
Over the past 30 years, a geographic contraction of the southern range edge of this species has occurred, with a northward latitudinal shift of approximately 1,250 km. Additionally, a more restricted distributional decline was recorded in the Bay of Biscay. Coastal SST warming data over the last three decades revealed a significant increase in temperature along most of the studied coastline, averaging 0.214°C/decade. Importantly, the analysis of existing and extinct population samples clearly distinguished two genetically different groups, a northern and a southern clade. Because of the range contraction, the southern group is currently represented by very few extant populations. This southern edge range shift is thus causing the loss of a distinct component of the species genetic background.
We reveal a climate-correlated diversity loss below the species level, a process that could render the species more vulnerable to future environmental changes and affect its evolutionary potential. This is a remarkable case of genetic uniqueness of a vanishing cryptic genetic clade (southern clade).
最近的全球气候变化已经在多种生态系统中产生了显著影响,物种分布范围发生了变化,但很少有证据表明这些变化与物种遗传库的变化有关。北非和北伊比利亚之间的大西洋海岸是研究物种分布与气候变化之间关系的理想场所,因为它包括了大量冷水和温水物种的分布极限。我们比较了藤壶的分布随时间的变化与历史上的海面温度(SST)模式,以确定范围变化与当代气候变化之间的联系。此外,我们用微卫星标记物对以前采样的灭绝和现存种群进行了遗传特征分析,以估计由此产生的隐性遗传侵蚀。
在过去的 30 年中,该物种的南部范围边缘发生了地理收缩,纬度向北移动了大约 1250 公里。此外,比斯开湾的分布范围下降更为明显。过去三十年来的沿海 SST 变暖数据显示,大部分研究海岸线的温度显著升高,平均每十年升高 0.214°C。重要的是,对现存和灭绝种群样本的分析清楚地区分了两个遗传上不同的群体,一个是北方群体,另一个是南方群体。由于范围收缩,目前南部群体仅由极少数现存种群代表。因此,这种南部边缘范围的变化导致了该物种遗传背景的一个独特组成部分的丧失。
我们揭示了一个与气候相关的物种水平以下的多样性损失过程,这种过程可能使物种更容易受到未来环境变化的影响,并影响其进化潜力。这是一个明显的例子,说明了一个正在消失的隐性遗传分支(南部分支)的遗传独特性。