Ancient Atmospheric Lead Pollution
In the early 90s, evidence was found in ice cores taken from Greenland of increased levels of ancient atmospheric lead, preserved by way of the annual precipitation that eventually formed into ice sheets. Since that time, similar records of atmospheric lead pollution have been uncovered in myriad ot...
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ftqueensunivojs:oai:library.queensu.ca/ojs:article/8388 2023-05-15T16:29:45+02:00 Ancient Atmospheric Lead Pollution Varaschin, Julian 2016-02-05 https://ojs.library.queensu.ca/index.php/inquiryatqueens/article/view/8388 unknown Queen's University https://ojs.library.queensu.ca/index.php/inquiryatqueens/article/view/8388 Inquiry@Queen's Undergraduate Research Conference Proceedings; 2010: 4th I@Q Conference Proceedings 2563-8912 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftqueensunivojs 2023-02-05T19:15:12Z In the early 90s, evidence was found in ice cores taken from Greenland of increased levels of ancient atmospheric lead, preserved by way of the annual precipitation that eventually formed into ice sheets. Since that time, similar records of atmospheric lead pollution have been uncovered in myriad other naturally forming deposits, including lake sediments and bogs. These records of lead pollution are presumed to reflect an increase in anthropogenic atmospheric lead pollution as metal became more heavily utilized by ancient peoples. This pollution confirmed for many the size and sophistication of the Roman economy. The records exhibit a clear peak around the beginning of the first millennium, roughly the midpoint of the Roman Empire and such levels were not seen again until after the industrial revolution was well underway. This peak in atmospheric lead is thought to show the climax of Roman Industry, followed by a subsequent decline and historians and scientists have sought to use this evidence as a proxy for the ancient world economy, but more specifically for the so called rise and fall of the Roman Empire. This presentation will explore the science behind linking the atmospheric lead pollution to Roman mining activities and why lead pollution is so strongly thought to reflect the roman economy. Alternative theories as to how atmospheric lead was produced in such quantities will be explored, including, increased agriculture and wood burning. Lastly, confounding factors will be considered such as volcanism and other ancient sources, including mining in Asia Minor and Han China. Article in Journal/Newspaper Greenland Queen's University, Ontario: OJS@Queen's University Greenland Inquiry@Queen's Undergraduate Research Conference Proceedings |
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Queen's University, Ontario: OJS@Queen's University |
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In the early 90s, evidence was found in ice cores taken from Greenland of increased levels of ancient atmospheric lead, preserved by way of the annual precipitation that eventually formed into ice sheets. Since that time, similar records of atmospheric lead pollution have been uncovered in myriad other naturally forming deposits, including lake sediments and bogs. These records of lead pollution are presumed to reflect an increase in anthropogenic atmospheric lead pollution as metal became more heavily utilized by ancient peoples. This pollution confirmed for many the size and sophistication of the Roman economy. The records exhibit a clear peak around the beginning of the first millennium, roughly the midpoint of the Roman Empire and such levels were not seen again until after the industrial revolution was well underway. This peak in atmospheric lead is thought to show the climax of Roman Industry, followed by a subsequent decline and historians and scientists have sought to use this evidence as a proxy for the ancient world economy, but more specifically for the so called rise and fall of the Roman Empire. This presentation will explore the science behind linking the atmospheric lead pollution to Roman mining activities and why lead pollution is so strongly thought to reflect the roman economy. Alternative theories as to how atmospheric lead was produced in such quantities will be explored, including, increased agriculture and wood burning. Lastly, confounding factors will be considered such as volcanism and other ancient sources, including mining in Asia Minor and Han China. |
format |
Article in Journal/Newspaper |
author |
Varaschin, Julian |
spellingShingle |
Varaschin, Julian Ancient Atmospheric Lead Pollution |
author_facet |
Varaschin, Julian |
author_sort |
Varaschin, Julian |
title |
Ancient Atmospheric Lead Pollution |
title_short |
Ancient Atmospheric Lead Pollution |
title_full |
Ancient Atmospheric Lead Pollution |
title_fullStr |
Ancient Atmospheric Lead Pollution |
title_full_unstemmed |
Ancient Atmospheric Lead Pollution |
title_sort |
ancient atmospheric lead pollution |
publisher |
Queen's University |
publishDate |
2016 |
url |
https://ojs.library.queensu.ca/index.php/inquiryatqueens/article/view/8388 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
Inquiry@Queen's Undergraduate Research Conference Proceedings; 2010: 4th I@Q Conference Proceedings 2563-8912 |
op_relation |
https://ojs.library.queensu.ca/index.php/inquiryatqueens/article/view/8388 |
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Inquiry@Queen's Undergraduate Research Conference Proceedings |
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