Map of Roman Republic in 1st century BCE (from Pinterest). |
If like me, you’re a bit shaky on that era, I’ll begin with a quickie on the affected transitions. Squeezing centuries into a handful of paragraphs and focusing on dates, I’ve omitted a wealth of important background, such as the relationship between Cleopatra and Julius Caesar.
Historic Background
The Late Period of Ancient Egyptian history ended in 332 BCE, when the Greeks conquered Egypt. The Greeks formed the Ptolemaic Kingdom in 305 BCE, and the Ptolemaic dynasty ruled Egypt until the Romans took control in 30 BCE, with the death of Cleopatra, the last Ptolemaic queen. Despite controlling Egypt for nearly three centuries, the Ptolemaic dynasty never became Egyptian, instead, isolating themselves in Alexandria.
Bronze statue of Julius Caesar located at the Roman Forum in Rome (from cestmoi.ca/en/bronze-statue-of-julius-caesar-in-rome/). |
Caesar was assassinated on the Ides of March, 44 BCE. His death triggered a 17-year power struggle that ultimately ended the Roman Republic and led, in 27 BCE, to the Roman Empire. The Empire would be ruled by a series of Emperors and expand its rule in Asia and Africa.
The political transitions in Rome and Egypt in the 40’s BCE were exacerbated by a period of unusually cold climate, crop failures, famine and disease in the Mediterranean region.
Documenting the Volcano
The study was conducted by an international, multidisciplinary team of 20 researchers, led by the Desert Research Institute, Reno, Nev. The team determined that the climate-related impacts were caused by eruptions of the Okmok volcano some 6,000 miles away in Alaska.
World map showing Okmok volcano in the Alaskan Aleutian Islands, Rome and Alexandria. |
Members of the team collected corroborating evidence from around the globe, including tree-ring-based climate records from Scandinavia, Austria and California, and climate records from cave formations in China.
The climate proxy records indicated that 43 and 42 BCE were among the coldest years of the recent millennia in the Northern Hemisphere at the start of one of the coldest decades. Modeling also suggested that the high-latitude eruption led to pronounced changes in hydroclimate, including seasonal temperatures in Mediterranean region as much as 7°C (13°F) below normal during the 2 years following the second eruption.
The team matched the scientific findings with written and archaeological descriptions of the eruption’s impact, including the failure of the Nile River to flood and the unrest in the region.
The Okmok volcano caldera in 2013; the summit of the cone formed during the 2008 eruption is eroding and a lake is filling the crater’s bottom (photo by J.R.G. Schaefer, from Alaska Volcano Observatory, Alaska Division of Geological & Geophysical Surveys, avo.alaska.edu/images/image.php?id=54161). |
Many different factors contributed to the fall of the Roman Republic and Ptolemaic Kingdom; however, the climatic effects of the 43 BCE Okmok eruption played an undeniably large role. Identifying and characterizing the volcanic source and eruption fills a knowledge gap that long puzzled archaeologists and historians.
Thanks for stopping by.
P.S.
Example sources of Roman and Ptolemaic history:
www.britannica.com/place/Roman-Republic
www.historycrunch.com/republic-vs-empire-in-ancient-rome.html#/
en.wikipedia.org/wiki/Roman_Republic
en.wikipedia.org/wiki/Roman_Empire
www.ancient.eu/Ptolemaic_Dynasty/
en.wikipedia.org/wiki/Ptolemaic_Kingdom
Study of effects of Okmok volcano eruption in Proc. of National Academy of Sciences of USA: www.pnas.org/content/early/2020/06/25/2002722117
Articles on study on EurekAlert! and Science websites:
eurekalert.org/pub_releases/2020-06/yu-cca062220.php
www.sciencemag.org/news/2020/06/alaskan-mega-eruption-may-have-helped-end-roman-republic
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