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Lead pollution recorded in Greenland ice indicates European emissions tracked plagues, wars, and imperial expansion during antiquity

  • Joseph R. McConnell (Corresponding author)
  • , Andrew I. Wilson
  • , Andreas Stohl
  • , Monica M. Arienzo
  • , Nathan J. Chellman
  • , Sabine Eckhardt
  • , Elisabeth M. Thompson
  • , A. Mark Pollard
  • , Jørgen Peder Steffensen

Publications: Contribution to journalArticlePeer Reviewed

Abstract

Lead pollution in Arctic ice reflects midlatitude emissions from ancient lead–silver mining and smelting. The few reported measurements have been extrapolated to infer the performance of ancient economies, including comparisons of economic productivity and growth during the Roman Republican and Imperial periods. These studies were based on sparse sampling and inaccurate dating, limiting understanding of trends and specific linkages. Here we show, using a precisely dated record of estimated lead emissions between 1100 BCE and 800 CE derived from subannually resolved measurements in Greenland ice and detailed atmospheric transport modeling, that annual European lead emissions closely varied with historical events, including imperial expansion, wars, and major plagues. Emissions rose coeval with Phoenician expansion, accelerated during expanded Carthaginian and Roman mining primarily in the Iberian Peninsula, and reached a maximum under the Roman Empire. Emissions fluctuated synchronously with wars and political instability particularly during the Roman Republic, and plunged coincident with two major plagues in the second and third centuries, remaining low for >500 years. Bullion in silver coinage declined in parallel, reflecting the importance of lead–silver mining in ancient economies. Our results indicate sustained economic growth during the first two centuries of the Roman Empire, terminated by the second-century Antonine plague.

Original languageEnglish
Pages (from-to)5726-5731
Number of pages6
JournalProceedings of the National Academy of Sciences of the United States of America
Volume115
Issue number22
DOIs
Publication statusPublished - 29 May 2018

Funding

ACKNOWLEDGMENTS. We thank S. Bernard and M. Legrand for helpful comments; R. Kreidberg for editorial assistance; the North Greenland Ice Core Project (NGRIP) community for providing ice-core samples; and students in the Desert Research Institute ice-core laboratory for their assistance. Analysis and interpretation of archived NGRIP2 ice-core samples were supported by the John Fell Oxford University Press Research Fund and All Souls College, Oxford, We thank S. Bernard and M. Legrand for helpful comments; R. Kreidberg for editorial assistance; the North Greenland Ice Core Project (NGRIP) community for providing ice-core samples; and students in the McConnell et al. Desert Research Institute ice-core laboratory for their assistance. Analysis and interpretation of archived NGRIP2 ice-core samples were supported by the John Fell Oxford University Press Research Fund and All Souls College, Oxford, as well as the Desert Research Institute. NGRIP is a multinational research program funded by participating institutions in Denmark, Germany, Japan, Sweden, Switzerland, France, Belgium, Iceland, and the United States.

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 8 - Decent Work and Economic Growth
    SDG 8 Decent Work and Economic Growth
  2. SDG 16 - Peace, Justice and Strong Institutions
    SDG 16 Peace, Justice and Strong Institutions

Austrian Fields of Science 2012

  • 105206 Meteorology

Keywords

  • Antiquity
  • Ice core
  • lead pollution
  • Plague
  • War

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