Neubauer Thomas A, Gofas Serge, Harzhauser Mathias
SNSB - Bavarian State Collection for Palaeontology and Geology, Richard-Wagner-Straße 10, 80333, Munich, Germany.
Department of Earth and Environmental Sciences, Palaeontology & Geobiology, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, 80333, Munich, Germany.
Sci Rep. 2025 Jul 1;15(1):20304. doi: 10.1038/s41598-025-06473-0.
Unveiling the processes that lead to biogeographic regionalisation is key to understanding the links between micro- and macroevolution, community processes and macroecology. However, many studies focus on present-day conditions while neglecting geological and palaeontological history. Here, we review the relevance of contemporary climatic conditions and ocean circulation patterns and their geological legacy on the distribution of marine benthic biota, using Mollusca as a model group. Based on global gridded occurrence data, we computed hierarchical cluster analyses and non-metric multidimensional scalings using Simpson's distance index at three systematic ranks (species, genus, family). Generalised additive models were applied to assess the relationship between taxon distribution and global sea-surface temperature. In addition, we introduce a novel method to quantify the geographic coherence of clusters identified by cluster analysis to ascertain biogeographically meaningful interpretation. We show that contemporary climate and palaeogeographic changes, which have shaped ocean circulation patterns over geological time, have had a significant impact on the global distribution of benthic shallow-water marine molluscs. Our results indicate a high level of provincialism for species, slightly less so for genera, and a polar vs. circum-temperate-tropical structure for families. The biogeographic units defined by our cluster analyses match existing ocean currents for species, while the poorer regionalisation for genus- and family-level data is the result of geologically young seaways or land bridges. Our findings evidence the importance of considering historical processes for the biogeography of modern faunas.
揭示导致生物地理区域化的过程是理解微观和宏观进化、群落过程与宏观生态学之间联系的关键。然而,许多研究关注的是当今的状况,却忽略了地质和古生物学历史。在此,我们以软体动物作为模型类群,综述当代气候条件和海洋环流模式及其地质遗留对海洋底栖生物区系分布的相关性。基于全球网格化的出现数据,我们在三个系统分类等级(物种、属、科)上使用辛普森距离指数进行了层次聚类分析和非度量多维尺度分析。应用广义相加模型来评估分类单元分布与全球海表温度之间的关系。此外,我们引入了一种新方法来量化聚类分析所识别聚类的地理连贯性,以确定具有生物地理意义的解释。我们表明,在地质时期塑造了海洋环流模式的当代气候和古地理变化,对底栖浅水海洋软体动物的全球分布产生了重大影响。我们的结果表明,物种的地方特有性程度很高,属的程度稍低,而科级则呈现极地与环温带 - 热带的结构。我们聚类分析所定义的生物地理单元与物种层面的现有洋流相匹配,而属级和科级数据的区域化较差是地质时期较年轻的海峡或陆桥造成的。我们的研究结果证明了考虑历史过程对现代动物群生物地理学的重要性。