1. Sedimentary ancient DNA shows terrestrial plant richness continuously increased over the Holocene in northern Fennoscandia
- Author
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Iva Pitelkova, Dilli Prasad Rijal, Tomasz Goslar, Youri Lammers, Nigel G. Yoccoz, Karin F. Helmens, Inger Greve Alsos, Francisco Javier Ancin Murguzur, Torbjørn Alm, Kari Anne Bråthen, Mary E. Edwards, Peter D. Heintzman, Antony G. Brown, Kelsey Lorberau, Jostein Bakke, J. Sakari Salonen, and Department of Geosciences and Geography
- Subjects
0106 biological sciences ,1171 Geosciences ,010506 paleontology ,010504 meteorology & atmospheric sciences ,Climate Change ,ved/biology.organism_classification_rank.species ,Annan geovetenskap och miljövetenskap ,Climate change ,medicine.disease_cause ,010603 evolutionary biology ,01 natural sciences ,Nutrient ,Effects of global warming ,Pollen ,Terrestrial plant ,medicine ,Humans ,DNA, Ancient ,Research Articles ,Ecosystem ,Holocene ,1172 Environmental sciences ,VDP::Mathematics and natural science: 400 ,0105 earth and related environmental sciences ,Multidisciplinary ,Ecology ,ved/biology ,Plant Sciences ,SciAdv r-articles ,VDP::Matematikk og Naturvitenskap: 400 ,Plants ,15. Life on land ,Lakes ,Geography ,Ancient DNA ,13. Climate action ,Species richness ,Other Earth and Related Environmental Sciences ,Research Article - Abstract
SedaDNA reveals regional climate and bedrock nutrients as major drivers of terrestrial plant diversity in northern Fennoscandia., The effects of climate change on species richness are debated but can be informed by the past. Here, we generated a sedimentary ancient DNA dataset covering 10 lakes and applied novel methods for data harmonization. We assessed the impact of Holocene climate changes and nutrients on terrestrial plant richness in northern Fennoscandia. We find that richness increased steeply during the rapidly warming Early Holocene. In contrast to findings from most pollen studies, we show that richness continued to increase thereafter, although the climate was stable, with richness and the regional species pool only stabilizing during the past three millennia. Furthermore, overall increases in richness were greater in catchments with higher soil nutrient availability. We suggest that richness will increase with ongoing warming, especially at localities with high nutrient availability and assuming that human activity remains low in the region, although lags of millennia may be expected.
- Published
- 2021