Živković Tatjana, Carrell Alyssa A, Granath Gustaf, Shaw A Jonathan, Pelletier Dale A, Schadt Christopher W, Klingeman Dawn M, Nilsson Mats B, Helbig Manuel, Warshan Denis, Klarenberg Ingeborg J, Gilbert Daniel, Kostka Joel E, Weston David J
Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA.
Department of Biology, Dalhousie University, Halifax, Nova Scotia, Canada.
Glob Chang Biol. 2025 Feb;31(2):e70066. doi: 10.1111/gcb.70066.
Sphagnum moss is the dominant plant genus in northern peatlands responsible for long-term carbon accumulation. Sphagnum hosts diverse microbial communities (microbiomes), and its phytobiome (plant host + constituent microbiome + environment) plays a key role in nutrient acquisition along with carbon cycling. Climate change can modify the Sphagnum-associated microbiome, resulting in enhanced host growth and thermal acclimation as previously shown in warming experiments. However, the extent of microbiome benefits to the host and the influence of host-microbe specificity on Sphagnum thermal acclimation remain unclear. Here, we extracted Sphagnum microbiomes from five donor species of four peatland warming experiments across a latitudinal gradient and applied those microbiomes to three germ-free Sphagnum species grown across a range of temperatures in the laboratory. Using this experimental system, we test if Sphagnum's growth response to warming depends on the donor and/or recipient host species, and we determine how the microbiome's growth conditions in the field affect Sphagnum host growth across a range of temperatures in the laboratory. After 4 weeks, we found that the highest growth rate of recipient Sphagnum was observed in treatments of matched host-microbiome pairs, with rates approximately 50% and 250% higher in comparison to maximum growth rates of non-matched host-microbiome pairs and germ-free Sphagnum, respectively. We also found that the maximum growth rate of host-microbiome pairs was reached when treatment temperatures were close to the microbiome's native temperatures. Our study shows that Sphagnum's growth acclimation to temperature is partially controlled by its constituent microbiome. Strong Sphagnum host-microbiome species specificity indicates the existence of underlying, unknown physiological mechanisms that may drive Sphagnum's ability to acclimatize to elevated temperatures. Together with rapid acclimation of the microbiome to warming, these specific microbiome-plant associations have the potential to enhance peatland resilience in the face of climate change.
泥炭藓是北方泥炭地中负责长期碳积累的优势植物属。泥炭藓拥有多样的微生物群落(微生物组),其植物微生物组(植物宿主+组成微生物组+环境)在养分获取以及碳循环中起着关键作用。气候变化可改变与泥炭藓相关的微生物组,如先前在变暖实验中所示,这会导致宿主生长增强和热适应。然而,微生物组对宿主的益处程度以及宿主-微生物特异性对泥炭藓热适应的影响仍不清楚。在此,我们从四个泥炭地暖化实验的五个供体物种中提取了泥炭藓微生物组,这些实验跨越了纬度梯度,并将这些微生物组应用于在实验室一系列温度下生长的三种无菌泥炭藓物种。利用这个实验系统,我们测试泥炭藓对变暖的生长反应是否取决于供体和/或受体宿主物种,并确定微生物组在野外的生长条件如何影响实验室一系列温度下泥炭藓宿主的生长。4周后,我们发现,在宿主-微生物组匹配对的处理中观察到受体泥炭藓的最高生长速率,与不匹配的宿主-微生物组对和无菌泥炭藓的最大生长速率相比,分别高出约50%和250%。我们还发现,当处理温度接近微生物组的原生温度时,宿主-微生物组对达到最大生长速率。我们的研究表明,泥炭藓对温度的生长适应部分由其组成微生物组控制。强烈的泥炭藓宿主-微生物组物种特异性表明存在潜在的、未知的生理机制,这些机制可能驱动泥炭藓适应升高温度的能力。连同微生物组对变暖的快速适应,这些特定的微生物组-植物关联有潜力增强泥炭地面对气候变化的恢复力。