Stomatal proxy record of CO2 concentrations from the last termination suggests an important role for CO2 at climate change transitions

A new stomatal proxy-based record of CO 2 concentrations ([CO 2 ]), based on Betula nana (dwarf birch) leaves from the Hässeldala Port sedimentary sequence in south-eastern Sweden, is presented. The record is of high chronological resolution and spans most of Greenland Interstadial 1 (GI-1a to 1c, A...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Steinthorsdottir, Margaret, Wohlfarth, Barbara, Kylander, Malin E., Blaauw, Maarten, Reimer, Paula J.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
/dk/atira/pure/sustainabledevelopmentgoals/climate_action
name=SDG 13 - Climate Action
Greenland
Betula nana
Dwarf birch
Online Access:https://pure.qub.ac.uk/en/publications/c378a0e0-8e39-40bf-97db-a5f6ab92d7cd
https://doi.org/10.1016/j.quascirev.2013.02.003
Description
Summary:A new stomatal proxy-based record of CO 2 concentrations ([CO 2 ]), based on Betula nana (dwarf birch) leaves from the Hässeldala Port sedimentary sequence in south-eastern Sweden, is presented. The record is of high chronological resolution and spans most of Greenland Interstadial 1 (GI-1a to 1c, Allerød pollen zone), Greenland Stadial 1 (GS-1, Younger Dryas pollen zone) and the very beginning of the Holocene (Preboreal pollen zone). The record clearly demonstrates that i) [CO 2 ] were significantly higher than usually reported for the Last Termination and ii) the overall pattern of CO 2 evolution through the studied time period is fairly dynamic, with significant abrupt fluctuations in [CO 2 ] when the climate moved from interstadial to stadial state and vice versa. A new loss-on-ignition chemical record (used here as a proxy for temperature) lends independent support to the Hässeldala Port [CO 2 ] record. The large-amplitude fluctuations around the climate change transitions may indicate unstable climates and that " tipping-point" situations were involved in Last Termination climate evolution. The scenario presented here is in contrast to [CO 2 ] records reconstructed from air bubbles trapped in ice, which indicate lower concentrations and a gradual, linear increase of [CO 2 ] through time. The prevalent explanation for the main climate forcer during the Last Termination being ocean circulation patterns needs to re-examined, and a larger role for atmospheric [CO 2 ] considered.

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