Suppr超能文献

末次冰消期化石孢粉组合的气候与系统发育群落结构之间的关系并非一成不变。

Relationships between climate and phylogenetic community structure of fossil pollen assemblages are not constant during the last deglaciation.

机构信息

University of Maryland Center for Environmental Science, Appalachian Lab, Frostburg, Maryland, United States of America.

出版信息

PLoS One. 2021 Jul 8;16(7):e0240957. doi: 10.1371/journal.pone.0240957. eCollection 2021.

Abstract

Disentangling the influence of environmental drivers on community assembly is important to understand how multiple processes influence biodiversity patterns and can inform understanding of ecological responses to climate change. Phylogenetic Community Structure (PCS) is increasingly used in community assembly studies to incorporate evolutionary perspectives and as a proxy for trait (dis)similarity within communities. Studies often assume a stationary relationship between PCS and climate, though few studies have tested this assumption over long time periods with concurrent community data. We estimated two PCS metrics-Nearest Taxon Index (NTI) and Net Relatedness index (NRI)-of fossil pollen assemblages of Angiosperms in eastern North America over the last 21 ka BP at 1 ka intervals. We analyzed spatiotemporal relationships between PCS and seven climate variables, evaluated the potential impact of deglaciation on PCS, and tested for the stability of climate-PCS relationships through time. The broad scale geographic patterns of PCS remained largely stable across time, with overdispersion tending to be most prominent in the central and southern portion of the study area and clustering dominating at the longitudinal extremes. Most importantly, we found that significant relationships between climate variables and PCS (slope) were not constant as climate changed during the last deglaciation and new ice-free regions were colonized. We also found weak, but significant relationships between both PCS metrics (i.e., NTI and NRI) and climate and time-since-deglaciation that also varied through time. Overall, our results suggest that (1) PCS of fossil Angiosperm assemblages during the last 21ka BP have had largely constant spatial patterns, but (2) temporal variability in the relationships between PCS and climate brings into question their usefulness in predictive modeling of community assembly.

摘要

解开环境驱动因素对群落组装的影响对于理解多种过程如何影响生物多样性模式,并为理解生态系统对气候变化的响应提供信息非常重要。系统发育群落结构(PCS)越来越多地被用于群落组装研究中,以纳入进化视角,并作为群落内部特征(相似性)的代理。研究通常假设 PCS 与气候之间存在固定关系,但很少有研究在有同时代群落数据的情况下,经过长时间来检验这种假设。我们在过去 21 千年内以 1 千年的间隔,估算了北美东部被子植物化石花粉组合的两个 PCS 度量-最近分类单元指数(NTI)和净亲缘关系指数(NRI)。我们分析了 PCS 与七个气候变量之间的时空关系,评估了冰川消退对 PCS 的潜在影响,并通过时间检验了气候-PCS 关系的稳定性。随着时间的推移,PCS 的广泛地理格局在很大程度上保持稳定,过度分散倾向于在研究区域的中部和南部最为突出,聚类在经度极端处占主导地位。最重要的是,我们发现,在过去的冰川消退期间,气候发生变化并出现新的无冰地区时,气候变量与 PCS(斜率)之间的显著关系并非是恒定的。我们还发现,两个 PCS 度量(即 NTI 和 NRI)与气候和冰川消退以来的时间之间存在微弱但显著的关系,并且这种关系也随着时间的推移而变化。总体而言,我们的研究结果表明,(1)过去 21 千年内化石被子植物组合的 PCS 具有大致稳定的空间格局,但(2)PCS 与气候之间的时间变化关系对其在群落组装的预测模型中的有用性提出了质疑。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验