Anthropogenic carbon release rate unprecedented during the past 66 million years

Richard E. Zeebe*, Andy Ridgwell, James C. Zachos

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

169 Citations (Scopus)
331 Downloads (Pure)

Abstract

Carbon release rates from anthropogenic sources reached a record high of ∼10 Pg C yr-1 in 2014. Geologic analogues from past transient climate changes could provide invaluable constraints on the response of the climate system to such perturbations, but only if the associated carbon release rates can be reliably reconstructed. The Palaeocene-Eocene Thermal Maximum (PETM) is known at present to have the highest carbon release rates of the past 66 million years, but robust estimates of the initial rate and onset duration are hindered by uncertainties in age models. Here we introduce a new method to extract rates of change from a sedimentary record based on the relative timing of climate and carbon cycle changes, without the need for an age model. We apply this method to stable carbon and oxygen isotope records from the New Jersey shelf using time-series analysis and carbon cycle-climate modelling. We calculate that the initial carbon release during the onset of the PETM occurred over at least 4,000 years. This constrains the maximum sustained PETM carbon release rate to less than 1.1 Pg C yr-1. We conclude that, given currently available records, the present anthropogenic carbon release rate is unprecedented during the past 66 million years. We suggest that such a 'no-analogue' state represents a fundamental challenge in constraining future climate projections. Also, future ecosystem disruptions are likely to exceed the relatively limited extinctions observed at the PETM.

Original languageEnglish
Pages (from-to)325-329
Number of pages5
JournalNature Geoscience
Volume9
Issue number4
Early online date21 Mar 2016
DOIs
Publication statusPublished - 1 Apr 2016

Keywords

  • Palaeoceanography
  • Palaeoclimate
  • Carbon cycle

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