The anthropogenic greenhouse era began thousands of years ago
The anthropogenic era is generally thought to have begun 150 to 200 years ago, when the industrial revolution began producing CO2 and CH4 at rates sufficient to alter their compositions in the atmosphere. A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmo...
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description | The anthropogenic era is generally thought to have begun 150 to 200 years ago, when the industrial revolution began producing CO2 and CH4 at rates sufficient to alter their compositions in the atmosphere. A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmospheric concentrations thousands of years ago. This hypothesis is based on three arguments. (1) Cyclic variations in CO2 and CH4 driven by Earth-orbital changes during the last 350,000 years predict decreases throughout the Holocene, but the CO2 trend began an anomalous increase 8000 years ago, and the CH4 trend did so 5000 years ago. (2) Published explanations for these mid- to late-Holocene gas increases based on natural forcing can be rejected based on paleoclimatic evidence. (3) A wide array of archeological, cultural, historical and geologic evidence points to viable explanations tied to anthropogenic changes resulting from early agriculture in Eurasia, including the start of forest clearance by 8000 years ago and of rice irrigation by 5000 years ago. In recent millennia, the estimated warming caused by these early gas emissions reached a global-mean value of ~0.8 degrees C and roughly 2 degrees C at high latitudes, large enough to have stopped a glaciation of northeastern Canada predicted by two kinds of climatic models. CO2 oscillations of ~10 ppm in the last 1000 years are too large to be explained by external (solar-volcanic) forcing, but they can be explained by outbreaks of bubonic plague that caused historically documented farm abandonment in western Eurasia. Forest regrowth on abandoned farms sequestered enough carbon to account for the observed CO2 decreases. Plague-driven CO2 changes were also a significant causal factor in temperature changes during the Little Ice Age (1300-1900 AD). |
doi_str_mv | 10.1023/B:CLIM.0000004577.17928.fa |
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A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmospheric concentrations thousands of years ago. This hypothesis is based on three arguments. (1) Cyclic variations in CO2 and CH4 driven by Earth-orbital changes during the last 350,000 years predict decreases throughout the Holocene, but the CO2 trend began an anomalous increase 8000 years ago, and the CH4 trend did so 5000 years ago. (2) Published explanations for these mid- to late-Holocene gas increases based on natural forcing can be rejected based on paleoclimatic evidence. (3) A wide array of archeological, cultural, historical and geologic evidence points to viable explanations tied to anthropogenic changes resulting from early agriculture in Eurasia, including the start of forest clearance by 8000 years ago and of rice irrigation by 5000 years ago. In recent millennia, the estimated warming caused by these early gas emissions reached a global-mean value of ~0.8 degrees C and roughly 2 degrees C at high latitudes, large enough to have stopped a glaciation of northeastern Canada predicted by two kinds of climatic models. CO2 oscillations of ~10 ppm in the last 1000 years are too large to be explained by external (solar-volcanic) forcing, but they can be explained by outbreaks of bubonic plague that caused historically documented farm abandonment in western Eurasia. Forest regrowth on abandoned farms sequestered enough carbon to account for the observed CO2 decreases. Plague-driven CO2 changes were also a significant causal factor in temperature changes during the Little Ice Age (1300-1900 AD).</description><identifier>ISSN: 0165-0009</identifier><identifier>EISSN: 1573-1480</identifier><identifier>DOI: 10.1023/B:CLIM.0000004577.17928.fa</identifier><identifier>CODEN: CLCHDX</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Agriculture ; Anthropogenic changes ; Anthropogenic factors ; Archaeology ; Atmospheric models ; Bubonic plague ; Carbon dioxide ; Carbon dioxide variations ; Climate change ; Climate models ; Climatology. Bioclimatology. Climate change ; Earth, ocean, space ; Emissions ; Exact sciences and technology ; External geophysics ; Farm buildings ; Farms ; Gases ; Glaciation ; Glaciology ; Greenhouse effect ; Holocene ; Hypotheses ; Ice ages ; Little Ice Age ; Meteorology ; Methane ; Monsoons ; Natural gas ; Oryza sativa ; Oscillations ; Pest outbreaks ; Plague ; Regrowth ; Rice ; Temperature changes ; Trends ; Wind</subject><ispartof>Climatic change, 2003-12, Vol.61 (3), p.261-293</ispartof><rights>2004 INIST-CNRS</rights><rights>Kluwer Academic Publishers 2003</rights><rights>Kluwer Academic Publishers 2003.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a669t-400d2b8832fee8d14c8e580ea722899d395c2d1510650654d8905d4da560177d3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15349795$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>RUDDIMAN, William F</creatorcontrib><title>The anthropogenic greenhouse era began thousands of years ago</title><title>Climatic change</title><description>The anthropogenic era is generally thought to have begun 150 to 200 years ago, when the industrial revolution began producing CO2 and CH4 at rates sufficient to alter their compositions in the atmosphere. A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmospheric concentrations thousands of years ago. This hypothesis is based on three arguments. (1) Cyclic variations in CO2 and CH4 driven by Earth-orbital changes during the last 350,000 years predict decreases throughout the Holocene, but the CO2 trend began an anomalous increase 8000 years ago, and the CH4 trend did so 5000 years ago. (2) Published explanations for these mid- to late-Holocene gas increases based on natural forcing can be rejected based on paleoclimatic evidence. (3) A wide array of archeological, cultural, historical and geologic evidence points to viable explanations tied to anthropogenic changes resulting from early agriculture in Eurasia, including the start of forest clearance by 8000 years ago and of rice irrigation by 5000 years ago. In recent millennia, the estimated warming caused by these early gas emissions reached a global-mean value of ~0.8 degrees C and roughly 2 degrees C at high latitudes, large enough to have stopped a glaciation of northeastern Canada predicted by two kinds of climatic models. CO2 oscillations of ~10 ppm in the last 1000 years are too large to be explained by external (solar-volcanic) forcing, but they can be explained by outbreaks of bubonic plague that caused historically documented farm abandonment in western Eurasia. Forest regrowth on abandoned farms sequestered enough carbon to account for the observed CO2 decreases. Plague-driven CO2 changes were also a significant causal factor in temperature changes during the Little Ice Age (1300-1900 AD).</description><subject>Agriculture</subject><subject>Anthropogenic changes</subject><subject>Anthropogenic factors</subject><subject>Archaeology</subject><subject>Atmospheric models</subject><subject>Bubonic plague</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide variations</subject><subject>Climate change</subject><subject>Climate models</subject><subject>Climatology. Bioclimatology. Climate change</subject><subject>Earth, ocean, space</subject><subject>Emissions</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Farm buildings</subject><subject>Farms</subject><subject>Gases</subject><subject>Glaciation</subject><subject>Glaciology</subject><subject>Greenhouse effect</subject><subject>Holocene</subject><subject>Hypotheses</subject><subject>Ice ages</subject><subject>Little Ice Age</subject><subject>Meteorology</subject><subject>Methane</subject><subject>Monsoons</subject><subject>Natural gas</subject><subject>Oryza sativa</subject><subject>Oscillations</subject><subject>Pest outbreaks</subject><subject>Plague</subject><subject>Regrowth</subject><subject>Rice</subject><subject>Temperature changes</subject><subject>Trends</subject><subject>Wind</subject><issn>0165-0009</issn><issn>1573-1480</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqF0ctqGzEUBmARGqib9h2GhDarcXV0l6GLxuQGDt2ka3EyOuML9owr2Yu8fTVOIFBILQkkxKcjoZ-xc-Bj4EJ-v5pMZ_cPY35oSls7BuuFG7d4wkagraxBOf6BjTgYXRfjP7JPOa-GlRVmxH48LqjCbrdI_bafU7dsqnki6hb9PlNFCasnmmNX7YYN7GKu-rZ6Jky5wnn_mZ22uM705XU-Y79vrh-nd_Xs1-399OesRmP8rlacR_HknBQtkYugGkfacUIrhPM-Sq8bEUEDN7oMFZ3nOqqI2nCwNsozdvlSd5v6P3vKu7BZ5obWa-yovCtYJTVY52WR3_4rBUgrofRjEBwXFsAch8o44Ad48Q9c9fvUlX8JwngNvphBnb-nwDutudO8oMkLalKfc6I2bNNyg-k5AA9D8OEqDMGHt-DDIfjQYjn89fUGzA2u24Rds8xvFbRU3not_wLwQase</recordid><startdate>20031201</startdate><enddate>20031201</enddate><creator>RUDDIMAN, William F</creator><general>Springer</general><general>Springer Nature B.V</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7XB</scope><scope>87Z</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8FL</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>F28</scope><scope>FR3</scope><scope>FRNLG</scope><scope>F~G</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H97</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>KL.</scope><scope>KR7</scope><scope>L.-</scope><scope>L.G</scope><scope>L6V</scope><scope>M0C</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>SOI</scope></search><sort><creationdate>20031201</creationdate><title>The anthropogenic greenhouse era began thousands of years ago</title><author>RUDDIMAN, William F</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a669t-400d2b8832fee8d14c8e580ea722899d395c2d1510650654d8905d4da560177d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Agriculture</topic><topic>Anthropogenic changes</topic><topic>Anthropogenic factors</topic><topic>Archaeology</topic><topic>Atmospheric models</topic><topic>Bubonic plague</topic><topic>Carbon dioxide</topic><topic>Carbon dioxide variations</topic><topic>Climate change</topic><topic>Climate models</topic><topic>Climatology. 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Climate change</topic><topic>Earth, ocean, space</topic><topic>Emissions</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Farm buildings</topic><topic>Farms</topic><topic>Gases</topic><topic>Glaciation</topic><topic>Glaciology</topic><topic>Greenhouse effect</topic><topic>Holocene</topic><topic>Hypotheses</topic><topic>Ice ages</topic><topic>Little Ice Age</topic><topic>Meteorology</topic><topic>Methane</topic><topic>Monsoons</topic><topic>Natural gas</topic><topic>Oryza sativa</topic><topic>Oscillations</topic><topic>Pest outbreaks</topic><topic>Plague</topic><topic>Regrowth</topic><topic>Rice</topic><topic>Temperature changes</topic><topic>Trends</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>RUDDIMAN, William F</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ABI/INFORM Collection</collection><collection>ABI/INFORM Global (PDF only)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ABI/INFORM Global (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ABI/INFORM Collection (Alumni Edition)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Business Premium Collection</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ANTE: Abstracts in New Technology & Engineering</collection><collection>Engineering Research Database</collection><collection>Business Premium Collection (Alumni)</collection><collection>ABI/INFORM Global (Corporate)</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Business Collection (Alumni Edition)</collection><collection>ProQuest Business Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - 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A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmospheric concentrations thousands of years ago. This hypothesis is based on three arguments. (1) Cyclic variations in CO2 and CH4 driven by Earth-orbital changes during the last 350,000 years predict decreases throughout the Holocene, but the CO2 trend began an anomalous increase 8000 years ago, and the CH4 trend did so 5000 years ago. (2) Published explanations for these mid- to late-Holocene gas increases based on natural forcing can be rejected based on paleoclimatic evidence. (3) A wide array of archeological, cultural, historical and geologic evidence points to viable explanations tied to anthropogenic changes resulting from early agriculture in Eurasia, including the start of forest clearance by 8000 years ago and of rice irrigation by 5000 years ago. In recent millennia, the estimated warming caused by these early gas emissions reached a global-mean value of ~0.8 degrees C and roughly 2 degrees C at high latitudes, large enough to have stopped a glaciation of northeastern Canada predicted by two kinds of climatic models. CO2 oscillations of ~10 ppm in the last 1000 years are too large to be explained by external (solar-volcanic) forcing, but they can be explained by outbreaks of bubonic plague that caused historically documented farm abandonment in western Eurasia. Forest regrowth on abandoned farms sequestered enough carbon to account for the observed CO2 decreases. Plague-driven CO2 changes were also a significant causal factor in temperature changes during the Little Ice Age (1300-1900 AD).</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1023/B:CLIM.0000004577.17928.fa</doi><tpages>33</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Agriculture Anthropogenic changes Anthropogenic factors Archaeology Atmospheric models Bubonic plague Carbon dioxide Carbon dioxide variations Climate change Climate models Climatology. Bioclimatology. Climate change Earth, ocean, space Emissions Exact sciences and technology External geophysics Farm buildings Farms Gases Glaciation Glaciology Greenhouse effect Holocene Hypotheses Ice ages Little Ice Age Meteorology Methane Monsoons Natural gas Oryza sativa Oscillations Pest outbreaks Plague Regrowth Rice Temperature changes Trends Wind |
title | The anthropogenic greenhouse era began thousands of years ago |
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