Biotic turnover rates during the Pleistocene-Holocene transition. (1st November 2016)

• Record Type: Journal Article
• Authors: Stivrins, Normunds; Soininen, Janne; Amon, Leeli; Fontana, Sonia L.; Gryguc, Gražyna; Heikkilä, Maija; Heiri, Oliver; Kisielienė, Dalia; Reitalu, Triin; Stančikaitė, Miglė; Veski, Siim; Seppä, Heikki
• Is Part Of: Quaternary science reviews. Volume 151(2016)
• Page Start: 100
• Page End: 110
• Publication Date: 2016-11-01
• Subjects: Temperature change -- Biotic turnover rates -- Regional extinctions -- Pollen -- Plant macrofossils -- Phytoplankton; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2016.09.008
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: The Northern Hemisphere is currently warming at the rate which is unprecedented during the Holocene. Quantitative palaeoclimatic records show that the most recent time in the geological history with comparable warming rates was during the Pleistocene-Holocene transition (PHT) about 14, 000 to 11, 000 years ago. To better understand the biotic response to rapid temperature change, we explore the community turnover rates during the PHT by focusing on the Baltic region in the southeastern sector of the Scandinavian Ice Sheet, where an exceptionally dense network on microfossil and macrofossil data that reflect the biotic community history are available. We further use a composite chironomid-based summer temperature reconstruction compiled specifically for our study region to calculate the rate of temperature change during the PHT. The fastest biotic turnover in the terrestrial and aquatic communities occurred during the Younger Dryas-Holocene shift at 11, 700 years ago. This general shift in species composition was accompanied by regional extinctions, including disappearance of mammoth ( Mammuthus primigenius ) and reindeer ( Rangifer tarandus ) and many arctic-alpine plant taxa, such as Dryas octopetala, Salix polaris and Saxifraga aizoides, from the region. This rapid biotic turnover rate occurred when the rate of warming was 0.17 °C/decade, thus slightly lower than the current Northern Hemisphere warming of 0.2 °C/decade. We therefore conclude that the Younger Dryas-Holocene shift with its rapid turnover rates and associated regional extinctions represents an important palaeoanalogue to the current high latitude warming and gives insights about the probable future turnover rates and patterns of the terrestrial and aquatic ecosystem change. Highlights: Biotic turnover rates for the Pleistocene-Holocene transition 14, 000–11, 000 years ago were estimated. Turnover rates were compared with a rate of temperature change record. Rapid warming and high biotic turnover 11, 700 years ago were accompanied by regional extinction of arctic-alpine species.