{"id":1671,"date":"2024-09-30T13:36:05","date_gmt":"2024-09-30T13:36:05","guid":{"rendered":"https:\/\/research.uga.edu\/team-research\/?post_type=projects&#038;p=1671"},"modified":"2025-09-19T20:54:15","modified_gmt":"2025-09-19T20:54:15","slug":"climax-was-chimborazo-volcano-ecuador-the-climate-modulator-leading-to-the-antonine-plague-in-the-roman-empire-during-the-second-century-ad","status":"publish","type":"projects","link":"https:\/\/research.uga.edu\/team-research\/projects\/climax-was-chimborazo-volcano-ecuador-the-climate-modulator-leading-to-the-antonine-plague-in-the-roman-empire-during-the-second-century-ad\/","title":{"rendered":"CLIMAX: Was Chimborazo volcano (Ecuador) the climate modulator leading to the Antonine Plague in the Roman Empire during the second century AD?"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><p>[vc_row css=&#8221;.vc_custom_1727290192326{margin-top: 0px !important;margin-right: 0px !important;margin-bottom: 0px !important;margin-left: 0px !important;padding-top: 0px !important;padding-right: 0px !important;padding-bottom: 0px !important;padding-left: 0px !important;}&#8221;][vc_column css=&#8221;.vc_custom_1579011887505{margin-top: 0px !important;margin-bottom: 0px !important;margin-left: 0px !important;padding-top: 0px !important;padding-bottom: 0px !important;padding-left: 0px !important;}&#8221;][vc_column_text css=&#8221;.vc_custom_1727290211804{margin-top: 0px !important;margin-left: 0px !important;padding-top: 0px !important;padding-left: 0px !important;}&#8221;]<\/p>\n<h1 class=\"site-title\"><span style=\"color: #ba0c2f;\">Teaming for Interdisciplinary Research Pre-Seed Program<\/span><\/h1>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row bg_type=&#8221;bg_color&#8221; css=&#8221;.vc_custom_1718395996651{margin-right: 0px !important;margin-bottom: 0px !important;border-right-width: 0px !important;border-bottom-width: 0px !important;padding-right: 0px !important;padding-bottom: 0px !important;background-color: #004e60 !important;}&#8221; bg_color_value=&#8221;#004e60&#8243;][vc_column width=&#8221;1\/2&#8243; css=&#8221;.vc_custom_1578671862861{background-color: #004e60 !important;}&#8221;][vc_column_text css=&#8221;.vc_custom_1719414238036{margin-left: 10px !important;}&#8221;]<\/p>\n<h3><span style=\"color: #ffffff;\">CLIMAX: Was Chimborazo volcano (Ecuador) the climate modulator leading to the Antonine Plague in the Roman Empire during the second century AD?<\/span><\/h3>\n<p>[\/vc_column_text][\/vc_column][vc_column width=&#8221;1\/2&#8243; css=&#8221;.vc_custom_1642018498769{margin-right: 0px !important;border-right-width: 0px !important;padding-right: 0px !important;}&#8221;][vc_single_image image=&#8221;926&#8243; img_size=&#8221;full&#8221; alignment=&#8221;right&#8221; css=&#8221;.vc_custom_1719416913003{margin-top: 0px !important;margin-right: 0px !important;margin-bottom: 0px !important;margin-left: 0px !important;border-right-width: 0px !important;padding-top: 0px !important;padding-right: 0px !important;padding-bottom: 0px !important;padding-left: 0px !important;background-color: #004e60 !important;}&#8221;][\/vc_column][\/vc_row][vc_row][vc_column css=&#8221;.vc_custom_1595855041843{margin-top: 0px !important;padding-top: 0px !important;}&#8221;][vc_row_inner][vc_column_inner width=&#8221;2\/3&#8243;][vc_empty_space][vc_column_text css=&#8221;&#8221;]CLIMAX is transdisciplinary research aimed to decode the interplay between climate change and large-scale eruption events by resolving the challenges of volcano-climate interaction, sub- surface processes leading to eruptions, and volcanic crisis preparedness and risk management at communities living in the shadow of active volcanoes. We aim to study the historical role of Chimborazo (Ecuador) as a volcano-induced climate crisis affecting the pre-Hispanic communities of Puruh\u00e1 and Incas and as one of the possible contributors to the Antonine plague that struck in the Roman Empire in the second century AD. Also, we aim to study the present-day Chimborazo volcano as a fragile mountainscape environment in which climate change-induced glacial ablation could lead to new natural hazards threatening the city of Riobamba and local communities (ca. 460,000 inhabitants within 30 km radius from the volcano).<\/p>\n<p>We propose to: a) correlate the age of the last eruption of Chimborazo assessed using radiocarbon analysis at CAIS, b) survey the volcano edifice and its ice cap instability zones and hazards using remote sensing techniques, c) modeling the interplay between climate dynamics, mountainscape, magma unrest, and eruption activity, and d) disseminating the project results via science communication, public outreach, conference abstracts, and publications.<\/p>\n<p>CLIMAX project is led by a transdisciplinary team of geologists, archeologists, geographers, climatologists, remote sensing scientists, landscape architects, environmental communicators, and tourism management scientists from UGA and ESPOCH (Ecuador). <u>Mattia Pistone<\/u> studies magma transport, eruption dynamics, and volatile cycles in the Earth\u2019s interior using a combination of experimental, analytical, and field-based approaches. The logistical organization of the CLIMAX field mission project will be facilitated by scientists <u>Carlos Renato Chavez Velasquez<\/u>, <u>Danny Daniel Castillo Vizuete<\/u>, <u>Alex Vinicio Gavilanes Montoya<\/u>, and <u>Christiam Aguirre<\/u> from ESPOCH. <u>Fausto Sarmiento<\/u> will catalyze the UGA-ESPOCH collaboration, generate the collection and export permits of samples, produce a counter-mapping of Chimborazo\u2019s local knowledge, and will assist during fieldwork for biocultural diversity and microsites refugia. <u>David Leigh<\/u> and <u>David Porinchu<\/u> are geography scientists specialized in climate changes and human impacts throughout the Holocene, including modern timescales. <u>Alexander Cherkinsky<\/u> is one of the PIs of the Calhoun Critical Zone Observatory with &gt;30 years of experience in carbon and stable isotope ratio analysis, including radiocarbon analyses of paleosols needed to establish the age of the eruptions at Chimborazo. <u>Jordan<\/u> <u>Pickett<\/u>, from UGA Classics, is an archaeologist and environmental historian, an expert in Roman historical texts and archaeology related to the Antonine Plague&#8217;s impacts in ancient Mediterranean society. <u>Kyle<\/u> <u>Woosnam<\/u> is specialized in managing and planning for nature-based tourism in rural amenity-rich regions; he will work in tandem with the ESPOCH scientists to determine the historical impact of Chimborazo on cultural ecosystem services among indigenous populations. <u>Jon Calabria<\/u> is a research leader in landscape architecture, conservation, and resiliency; he will assist with planning and site design activities to reduce impacts to human settlement from disturbances. <u>Anandam Kavoori<\/u> works at the intersection of science and storytelling, and has been a consultant to Discovery Channel, CNN international and Start TV. His expertise will greatly contribute to the science communication protocols of CLIMAX project, and will help reach different stakeholders and audiences and implement broader impacts of the proposed project.[\/vc_column_text][vc_gallery interval=&#8221;0&#8243; images=&#8221;978&#8243; img_size=&#8221;large&#8221; onclick=&#8221;img_link_large&#8221; custom_links_target=&#8221;_blank&#8221; css=&#8221;&#8221;][\/vc_column_inner][vc_column_inner width=&#8221;1\/3&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<h4>Team Lead<\/h4>\n<p><strong>Mattia Pistone<\/strong><br \/>\n<a href=\"mailto:mp77656@uga.edu\">mp77656@uga.edu<\/a><br \/>\nGeology<\/p>\n<h4>Team Members<\/h4>\n<p><strong>Jon Calabria<\/strong><br \/>\n<a href=\"mailto:jcalabr@uga.edu\">jcalabr@uga.edu<\/a><br \/>\nEnvironment + Design<br \/>\nEnvironment + Design<\/p>\n<p><strong>Anandam Kavoori<\/strong><br \/>\n<a href=\"mailto:akavoori@gmail.com\">akavoori@gmail.com<\/a><br \/>\nGrady<br \/>\nEntertain &amp; Media Stds<\/p>\n<p><strong>Jordan Pickett<\/strong><br \/>\n<a href=\"mailto:jordan.pickett@uga.edu\">jordan.pickett@uga.edu<\/a><br \/>\nFranklin<br \/>\nClassics<\/p>\n<p><strong>Fausto Sarmiento<\/strong><br \/>\n<a href=\"mailto:fsarmien@uga.edu\">fsarmien@uga.edu<\/a><br \/>\nFranklin<br \/>\nGeography<\/p>\n<p><strong>Kyle Woosnam<\/strong><br \/>\n<a href=\"mailto:woosnam@uga.edu\">woosnam@uga.edu<\/a><br \/>\nWarnell Forest<br \/>\nScience and Natural Resources<\/p>\n<p><strong>David Leigh<\/strong><br \/>\n<a href=\"mailto:dleigh@uga.edu\">dleigh@uga.edu<\/a><br \/>\nFranklin<br \/>\nGeography<\/p>\n<p><strong>David Porinchu<\/strong><br \/>\n<a href=\"mailto:porinchu@uga.edu\">porinchu@uga.edu<\/a><br \/>\nFranklin<br \/>\nGeography<\/p>\n<p><strong>Alexander Cherkinsky<\/strong><br \/>\n<a href=\"mailto:acherkin@uga.edu\">acherkin@uga.edu<\/a><br \/>\nCenter for Applied Isotope Studies<br \/>\nCenter for Applied Isotope Studies[\/vc_column_text][\/vc_column_inner][\/vc_row_inner][\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"featured_media":0,"menu_order":0,"template":"","format":"standard","meta":{"_links_to":"","_links_to_target":""},"categories":[],"class_list":["post-1671","projects","type-projects","status-publish","format-standard","hentry"],"_links":{"self":[{"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/projects\/1671"}],"collection":[{"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/projects"}],"about":[{"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/types\/projects"}],"version-history":[{"count":0,"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/projects\/1671\/revisions"}],"wp:attachment":[{"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/media?parent=1671"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/research.uga.edu\/team-research\/wp-json\/wp\/v2\/categories?post=1671"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}