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The Anthropogenic Greenhouse Era Began Thousands of Years Ago
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“Subsequent Holocene CO2 concentrations remained approximately stable, a very slow rise of 260 to 285 ppm from ~9000 B.P. (Fig. 5A) being ascribed to early human agriculture by some ( 3 ), albeit controversially ( 66 ).”
From The Anthropocene is functionally and stratigraphically distinct from the Holocene (2016) · cites this paper as [3]
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Items 101–200 of 1,658
Stratigraphy of the Anthropocene
Zalasiewicz, J., Williams, M., Fortey, R. A., Smith, A. Р., Barry, T. L., Coe, A. L., Bown, P. R., Rawson, P. F., Gale, A. S., Gibbard, P. L., et al. (2011) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2010.0315 · Cited by 229
Lowering carbon footprint of durum wheat by diversifying cropping systems
Gan, Y., Liang, C., Wang, X., & McConkey, B. G. (2011) · Field Crops Research · doi:10.1016/j.fcr.2011.03.020 · Cited by 214
Contributions of Quaternary botany to modern ecology and biogeography
Birks, H. J. B. (2019) · Plant Ecology & Diversity · doi:10.1080/17550874.2019.1646831 · Cited by 221
Separating Forced from Chaotic Climate Variability over the Past Millennium
Schurer, A., Hegerl, G. C., MANN, M. E., Tett, S. F. B., & Phipps, S. J. (2013) · Journal of Climate · doi:10.1175/jcli-d-12-00826.1 · Cited by 214
Was the Anthropocene anticipated?
Hamilton, C., & Grinevald, J. (2015) · The Anthropocene Review · doi:10.1177/2053019614567155 · Cited by 211
Strategies for reducing the carbon footprint of field crops for semiarid areas. A review
Gan, Y., Liang, C., Hamel, C., et al. (2011) · Agronomy for Sustainable Development · doi:10.1007/s13593-011-0011-7 · Cited by 208
“Scientific evidence suggests the Earth’s climate has recently been rapidly changing, largely due to increasing anthropogenic greenhouse gas (GHG) emissions (Ruddiman 2003; IPCC 2006).”
Backgroundde Boer, J., & Aiking, H. (2011) · Ecological Economics · doi:10.1016/j.ecolecon.2011.03.001 · Cited by 223
“With the introduction of early agriculture about 10,000 years ago humans started to make a unique imprint on the Earth (Ruddiman, 2003).”
BackgroundConservation in the Anthropocene
Caro, T., Darwin, J., Forrester, T. D., et al. (2011) · Conservation Biology · doi:10.1111/j.1523-1739.2011.01752.x · Cited by 205
“Indeed, the current epoch is now being referred to as the Anthropocene (Crutzen & Stoermer 2000), which has led geologists to formally debate stratigraphic evidence for this new phenomenon (Zalasiewicz et al. 2011) and to argue over not if but when it began (Ruddiman 2003).”
BackgroundHellman, S., Gaillard, M., Broström, A., et al. (2007) · Journal of Quaternary Science · doi:10.1002/jqs.1126 · Cited by 203
Human–environment interactions: learning from the past
Dearing, J. A., Battarbee, R. W., Dikau, R., Larocque, I., & Oldfield, F. (2006) · Regional Environmental Change · doi:10.1007/s10113-005-0011-8 · Cited by 205
Oxygen-18 of O 2 Records the Impact of Abrupt Climate Change on the Terrestrial Biosphere
Severinghaus, J. P., Beaudette, R., Headly, M. A., et al. (2009) · Science · doi:10.1126/science.1169473 · Cited by 199
Wolfe, A. P., Hobbs, W. O., Birks, H. H., Briner, J. P., Holmgren, S. U., Ingólfsson, Ó., Kaushal, S. S., Miller, G. H., Pagani, M., Saros, J. E., et al. (2013) · Earth-Science Reviews · doi:10.1016/j.earscirev.2012.11.001 · Cited by 190
“While there is no question that humans have strongly influenced the environment for millennia prior (Ruddiman, 2003), impacting both terrestrial and aquatic ecosystems (Birks, 1986; Renberg et al.”
BackgroundPlanetary Boundaries guide humanity’s future on Earth
Rockström, J., Donges, J. F., Fetzer, I., Martin, M. A., Wang‐Erlandsson, L., & Richardson, K. (2024) · Nature Reviews Earth & Environment · doi:10.1038/s43017-024-00597-z · Cited by 276
Hamilton, C. (2016) · The Anthropocene Review · doi:10.1177/2053019616634741 · Cited by 204
“…Ruddiman published a paper arguing that the Holocene–Anthropocene shift occurred not at the end of the 18th century with the Industrial Revolution but 5000–8000 years ago with the onset of forest clearing and farming, which led to enhanced levels of CO2 and CH4 in the atmosphere (Ruddiman, 2003).”
BackgroundHistorical soil erosion by water in Germany: Scales and archives, chronology, research perspectives
Dreibrodt, S., Lubos, C., Terhorst, B., et al. (2009) · Quaternary International · doi:10.1016/j.quaint.2009.06.014 · Cited by 189
Braje, T. J., & Erlandson, J. M. (2013) · Anthropocene · doi:10.1016/j.ancene.2013.08.003 · Cited by 197
Erkens, G., van der Meulen, M. J., & Middelkoop, H. (2016) · Hydrogeology Journal · doi:10.1007/s10040-016-1380-4 · Cited by 188
Effects of human land-use on the global carbon cycle during the last 6,000 years
Olofsson, J., & Hickler, T. (2007) · Vegetation History and Archaeobotany · doi:10.1007/s00334-007-0126-6 · Cited by 183
“Land-use changes result in biogeophysical climatic effects through modifications of surface albedo and roughness (Brovkin et al. 2006) and biogeochemical effects through, for example, alterations in vegetation and soil carbon pools (Houghton and Goodale 2004), which influence atmospheric greenhouse gas levels and glob…”
BackgroundResultInfluentialDiachronous beginnings of the Anthropocene: The lower bounding surface of anthropogenic deposits
Edgeworth, M., deB Richter, D., Waters, C., Haff, P., Neal, C., & Price, S. J. (2015) · The Anthropocene Review · doi:10.1177/2053019614565394 · Cited by 181
“Such evidence supports calls for an ‘early anthropogenic era’ (Ruddiman, 2003, 2013).”
BackgroundDubois, N., Saulnier‐Talbot, É., Mills, K., Gell, P., Battarbee, R. W., Bennion, H., Chawchai, S., Dong, X., Francus, P., Flower, R. J., et al. (2017) · The Anthropocene Review · doi:10.1177/2053019617740365 · Cited by 185
“…catchments with fertile soils have the longest history of human impact, dating from the start of primitive agriculture (following forest clearance), which is typically reflected by a decrease in tree pollen relative to herb and crop taxa (Birks et al., 1988; Räsänen et al., 2006; Ruddiman, 2003).”
BackgroundSoil carbon management and climate change
Lal, R. (2013) · Carbon Management · doi:10.4155/cmt.13.31 · Cited by 214
Food security in a changing climate
Lal, R. (2013) · Ecohydrology & Hydrobiology · doi:10.1016/j.ecohyd.2013.03.006 · Cited by 186
Sequestering carbon in soils of arid ecosystems
Lal, R. (2009) · Land Degradation and Development · doi:10.1002/ldr.934 · Cited by 184
“Emission of CH4 commenced with the cultivation of rice paddies and domestication of ruminants 5–8millennia ago (Ruddiman, 2003, 2005).”
BackgroundRose, N. L. (2015) · Environmental Science & Technology · doi:10.1021/acs.est.5b00543 · Cited by 178
Changing boreal methane sources and constant biomass burning during the last termination
Fischer, H., Behrens, M., Böck, M., Richter, U., Schmitt, J. H. M. M., Loulergue, L., Chappellaz, J., Spahni, R., Blunier, T., Leuenberger, M., et al. (2008) · Nature · doi:10.1038/nature06825 · Cited by 174
Methane emissions from the surface of the Three Gorges Reservoir
Chen, H., Yuan, X., Chen, Z., et al. (2011) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jd016244 · Cited by 174
Fire, climate change and biodiversity in Amazonia: a Late-Holocene perspective
Bush, M. B., Silman, M. R., McMichael, C., & Saatchi, S. (2008) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2007.0014 · Cited by 152
“At the other extreme, if all the seasonal forests of Amazonia were burning, there would have been significant impacts on both biodiversity and climate, i.e. contributing to the medieval warm period (sensu Ruddiman 2003).”
BackgroundTarasov, P. E., Bezrukova, E. V., Karabanov, E. B., et al. (2007) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2007.05.002 · Cited by 171
“8000 years already (Ruddiman, 2003) provides a temptation to find a relationship between the cultural periods and the phases with a more pronounced role of the steppe and meadow communities also around Lake Baikal.”
BackgroundCovariability of the Southern Westerlies and atmospheric CO2 during the Holocene
Moreno, P. I., Francois, J. P., Moy, C. M., & Villa-Martínez, R. P. (2010) · Geology · doi:10.1130/g30962.1 · Cited by 173
“, 2003), and land use changes (Ruddiman, 2003); however, no single mechanism has been able to account for the timing and structure of natural atmospheric CO2 changes during the Holocene.”
BackgroundXu, Q., Zhang, S., Gaillard, M., et al. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.07.017 · Cited by 167
Anthropogenic Influences on World Soils and Implications to Global Food Security
Lal, R. (2007) · Advances in agronomy · doi:10.1016/s0065-2113(06)93002-8 · Cited by 169
Soil carbon stocks under present and future climate with specific reference to European ecoregions
Lal, R. (2007) · Nutrient Cycling in Agroecosystems · doi:10.1007/s10705-007-9147-x · Cited by 165
“The impact of land use conversion and agricultural activities on CO2 abundance began with the onset of settled agriculture about 10,000 years ago (Ruddiman 2003).”
BackgroundHoffmann, T., Thorndycraft, V. R., Brown, A. G., et al. (2010) · Global and Planetary Change · doi:10.1016/j.gloplacha.2010.04.008 · Cited by 165
Late Holocene methane rise caused by orbitally controlled increase in tropical sources
Singarayer, J. S., Valdes, P. J., Friedlingstein, P., et al. (2011) · Nature · doi:10.1038/nature09739 · Cited by 164
“Specifically, our study addresses the issues of (1) whether natural processes explain the late-Holocene methane increase and the pre-Holocene methane record, (2) the main location of increased methane emissions during the late Holocene, and (3) the relative importance of different natural processes in producing glacia…”
BackgroundMethodInfluentialAllegories of the Anthropocene
DeLoughrey, E. (2019) · Duke University Press eBooks · doi:10.1215/9781478090021 · Cited by 289
Erosion under climate and human pressures: An alpine lake sediment perspective
Arnaud, F., Poulenard, J., Giguet‐Covex, C., Wilhelm, B., Révillon, S., Jenny, J., Revel, M., Enters, D., Bajard, M., Fouinat, L., et al. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.09.018 · Cited by 166
“It was argued that human-triggered erosion changes (Poirier et al., 2011), soil transformation (Certini and Scalenghe, 2011) or the effect of land-use on the carbon cycle (Ruddiman, 2003) could de fi ne the Anthropocene period itself.”
Land surface temperature changes in Northern Iberia since 4000yrBP, based on δ13C of speleothems
Martín‐Chivelet, J., Muñoz-García, M. B., Edwards, R. L., Jiménez, M. J. T., & Martínez, A. I. O. (2011) · Global and Planetary Change · doi:10.1016/j.gloplacha.2011.02.002 · Cited by 160
“, Robock, 1979; Crowley, 2000) and anthropogenic changes in forestation (Ruddiman, 2003).”
BackgroundSoil Science and the Carbon Civilization
Lal, R. (2007) · Soil Science Society of America Journal · doi:10.2136/sssaj2007.0001 · Cited by 166
“…(i) Will soil amplify climate change (Powlson, 2005) through positive feedback such as temperature sensitivity of organic matter decomposition (Ruddiman, 2003, 2005; Argen and Wetterstedt, 2007; Davidson and Janssens, 2006), increase in sensitivity of non-labile C (Briones et al., 2007), and…”
BackgroundDistinguishing the Roles of Natural and Anthropogenically Forced Decadal Climate Variability
Solomon, A. B., Goddard, L., Kumar, A., Carton, J. A., Deser, C., Fukumori, I., Greene, A. M., Hegerl, G. C., Kirtman, B. P., Kushnir, Y., et al. (2010) · Bulletin of the American Meteorological Society · doi:10.1175/2010bams2962.1 · Cited by 159
Marquer, L., Gaillard, M., Sugita, S., Trondman, A., Mazier, F., Nielsen, A. B., Fyfe, R., Odgaard, B. V., Alenius, T., Birks, H. J. B., et al. (2014) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2014.02.013 · Cited by 158
“Recent geochemical and modelling studies have suggested that the onset of significant anthropogenic impacts through forest clearance in some areas started even earlier, perhaps as long as 8000 years ago (Ruddiman, 2003; Kaplan et al., 2011; Ruddiman et al., 2011).”
BackgroundRiegl, B., Bruckner, A., Coles, S. L., Renaud, P. G., & Dodge, R. E. (2009) · Annals of the New York Academy of Sciences · doi:10.1111/j.1749-6632.2009.04493.x · Cited by 166
“There is general debate concerning exactly when the Anthropocene began (Crutzen and Steffen 2003; Ruddiman 2003), and for reefs we certainly do not know.”
BackgroundSchlütz, F., & Lehmkuhl, F. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.01.009 · Cited by 158
Current and future threats to human health in the Anthropocene
Tong, S., Bambrick, H., Beggs, P. J., Chen, L., Hu, Y., Ma, W., Steffen, W., & Tan, J. (2021) · Environment International · doi:10.1016/j.envint.2021.106892 · Cited by 175
Recarbonization of the Biosphere
Boike, J., Langer, M., Lantuit, H., Muster, S., Sachs, T., Ovderduin, P. P., Westermann, S., Roth, K., & McGuire, A. D. (2012) · Springer eBooks · doi:10.1007/978-94-007-4159-1 · Cited by 167
“Increase in atmospheric CO 2 concentration may have begun about 8,000 years ago and that of methane (CH 4 ) about 5,000 years ago corresponding with start of forest clearance and cultivation of irrigated rice paddies, respectively (Ruddiman 2003 ) .”
BackgroundInfluentialCandy, I., Schreve, D., Sherriff, J. E., & Tye, G. (2013) · Earth-Science Reviews · doi:10.1016/j.earscirev.2013.09.006 · Cited by 159
Fischer‐Kowalski, M., Krausmann, F., & Pallua, I. (2014) · The Anthropocene Review · doi:10.1177/2053019613518033 · Cited by 164
“Here, we also wish to question the notion that such a date should be determined by particular observable environmental impacts of the mode of human operation, as for example Ruddiman (2003, 2013) argues.”
BackgroundInfluentialCarbon cycle feedbacks and future climate change
Friedlingstein, P. (2015) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2014.0421 · Cited by 160
Constraints on the Late Holocene Anthropogenic Contribution to the Atmospheric Methane Budget
Mitchell, L., Brook, E., Lee, J. E., Buizert, C., & Sowers, T. (2013) · Science · doi:10.1126/science.1238920 · Cited by 136
Miehe, G., Miehe, S., Böhner, J., Kaiser, K., Hensen, I., Madsen, D. B., Liu, J., & Opgenoorth, L. (2014) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2013.12.004 · Cited by 151
Li, F., Gaillard, M., Cao, X., Herzschuh, U., Sugita, S., Tarasov, P. E., Wagner, M., Xu, Q., Ni, J., Wang, W., et al. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103119 · Cited by 150
“…quantification of anthropogenic landcover change (mainly deforestation) over the Holocene and its feedback effects on past climate remains a matter of debate (e.g. Ruddiman, 2003, 2005; Tarasov et al., 2006; Gaillard et al., 2010; Kleinen et al., 2011; Wagner et al., 2013; Ruddiman et al., 2016).”
BackgroundFire and human evolution: The deep-time blueprints of the Anthropocene
Glikson, A. Y. (2013) · Anthropocene · doi:10.1016/j.ancene.2014.02.002 · Cited by 147
Comparison between Holocene and Marine Isotope Stage-11 sea-level histories
Rohling, E. J., Braun, K., Grant, K., Kučera, M., Roberts, A. P., Siddall, M. E., & Trommer, G. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.12.054 · Cited by 150
“…should also be investigated in terms of changes in these feedback responses due to processes other than insolation, including controversial suggestions concerning man's long-term impacts from deforestation and CH4 and CO2 emissions (Ruddiman, 2003, 2005, 2006, 2007; Hansen et al., 2008).”
BackgroundEffect of per-capita land use changes on Holocene forest clearance and CO2 emissions
Ruddiman, W. F., & Ellis, E. C. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.05.022 · Cited by 141
“house-gas trends thousands of years ago because of emissions from early agriculture ( Ruddiman, 2003,”
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Pyrogeography and the Global Quest for Sustainable Fire Management
Bowman, D. M. J. S., O'Brien, J. A., & Goldammer, J. G. (2013) · Annual Review of Environment and Resources · doi:10.1146/annurev-environ-082212-134049 · Cited by 152
THE ANTHROPOCENE: ARE HUMANS NOW OVERWHELMING THE GREAT FORCES OF NATURE?
Steffen, W., Crutzen, P. J., & McNeill, J. R. (2019) · University of California Press eBooks · doi:10.1525/9780520964297-051 · Cited by 142
Formal subdivision of the Quaternary System/Period: Past, present, and future
Head, M. J., & Gibbard, P. L. (2015) · Quaternary International · doi:10.1016/j.quaint.2015.06.039 · Cited by 142
“This was originally highlighted by Ruddiman (2003) and recently re-emphasized by the same author (Ruddiman et al. 2015), who questioned the wisdom of selecting 1945 as the start of the “Anthropocene” when this would exclude extensive agricultural and early-industrial modifications such as…”
BackgroundEvidence from wavelet analysis for a mid-Holocene transition in global climate forcing
Debret, M., Sebag, D., Crosta, X., Masséi, N., Petit, J., Chapron, E., & Bout‐Roumazeilles, V. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.06.005 · Cited by 140
TURNEY, C. S. M., Palmer, J., Maslin, M. A., Hogg, A. G., Fogwill, C. J., Southon, J. R., Fenwick, P., Helle, G., Wilmshurst, J. M., McGlone, M. S., et al. (2018) · Scientific Reports · doi:10.1038/s41598-018-20970-5 · Cited by 136
The genic view of hybridization in the Anthropocene
Ottenburghs, J. (2021) · Evolutionary Applications · doi:10.1111/eva.13223 · Cited by 148
Science with Society in the Anthropocene
Seidl, R., Brand, F. S., Stauffacher, M., Krütli, P., Le, Q. B., Spörri, A., Meylan, G., Moser, C., González, M. B., & Scholz, R. W. (2013) · AMBIO · doi:10.1007/s13280-012-0363-5 · Cited by 140
“Paul Crutzen proposes that the Anthropocene Age started with the industrial revolution, and that phenomena such as the ozone hole and climate change now demonstrate that the human species can be regarded as a geological factor modifying the earth system (Ruddiman 2003, 2007).”
BackgroundPaleoecological Perspectives on Fire Ecology: Revisiting the Fire-Regime Concept
Whitlock, C. L., Higuera, P. E., McWethy, D. B., & Briles, C. E. (2010) · The Open Ecology Journal · Cited by 139
East, A. E., & Sankey, J. B. (2020) · Reviews of Geophysics · doi:10.1029/2019rg000692 · Cited by 156
Ward, P. J., van Balen, R. T., Verstraeten, G., et al. (2008) · Geomorphology · doi:10.1016/j.geomorph.2008.07.006 · Cited by 138
“In reality some centuries will have seen faster/slower rates of land use change, and the long-term deforestationmay at times even have been checked by external influences such as the bubonic plague (e.g. Lang et al., 2003; Ruddiman, 2003).”
BackgroundClimate-human-environment interactions: resolving our past
Dearing, J. A. (2006) · Climate of the past · doi:10.5194/cp-2-187-2006 · Cited by 136
“Ruddiman (2003) used archaeological, palaeoecological and historical records to support his hypothesis that the apparently anomalous www.clim-past.net/2/187/2006/ Clim.”
InfluentialFire in ice: two millennia of boreal forest fire history from the Greenland NEEM ice core
Zennaro, P., Kehrwald, N., McConnell, J. R., Schuepbach, S., Maselli, O. J., Marlon, J. R., Vallelonga, P., Leuenberger, D., Zangrando, R., Spolaor, A., et al. (2014) · Climate of the past · doi:10.5194/cp-10-1905-2014 · Cited by 147
“…practices (FAO, 2007) – practices which may have affected fire regimes during the entire past millennia (Bowman et al., 2009; Kaplan et al., 2011; Ruddiman, 2003) The observable impact of humans on fire regimes differs by geographic region (McWethy et al., 2009; Marlon et al., 2012; Power et…”
Maselli, V., & Trincardi, F. (2013) · Scientific Reports · doi:10.1038/srep01926 · Cited by 136
Schneider, R., Schmitt, J. H. M. M., Köhler, P., Joos, F., & Fischer, H. (2013) · Climate of the past · doi:10.5194/cp-9-2507-2013 · Cited by 146
Quaternary Sea-Level Changes: A Global Perspective
Murray‐Wallace, C. V., & Woodroffe, C. D. (2014) · Research Online (University of Wollongong) · Cited by 136
Measurement and prediction of enteric methane emission
Sejian, V., Lal, R., Lakritz, J., & Ezeji, T. C. (2010) · International Journal of Biometeorology · doi:10.1007/s00484-010-0356-7 · Cited by 136
“Release of CH4 into the atmosphere has been directly linked with the domestication of livestock 5,000 years ago (Ruddiman 2003).”
BackgroundGoldewijk, K. K., Dekker, S. C., & van Zanden, J. L. (2017) · Journal of Land Use Science · doi:10.1080/1747423x.2017.1354938 · Cited by 135
“As long as humans have walked the Earth, they have been altering the global landscape (Kaplan et al., 2011; Ruddiman, 2003).”
A movable trigger: Fossil fuel CO2 and the onset of the next glaciation
Archer, D. E., & Ganopolski, A. (2005) · Geochemistry Geophysics Geosystems · doi:10.1029/2004gc000891 · Cited by 134
“Paillard’s i0 was a somewhat arbitrary choice within a wide range of acceptable values, however, and a slight change in i0 could easily tip the simulation into the onset of glaciation now rather than in 50 kyr.”
BackgroundThe Columbian Encounter and the Little Ice Age: Abrupt Land Use Change, Fire, and Greenhouse Forcing
Dull, R. A., Nevle, R. J., Woods, W. I., Bird, D. K., Avnery, S., & Denevan, W. M. (2010) · Annals of the Association of American Geographers · doi:10.1080/00045608.2010.502432 · Cited by 141
“Although the pollen record is crucial to our understanding of prehistoric land use practices, as are studies of stable carbon isotopes of organic matter in sediments (Dull 2004; Lane et al. 2009), we contend that the most compelling suite of available evidence in support of the pre-Columbian Anthropocene hypothesis co…”
BackgroundInfluentialResponses of Temperate Forest Productivity to Insect and Pathogen Disturbances
Flower, C. E., & Gonzàlez‐Meler, M. A. (2015) · Annual Review of Plant Biology · doi:10.1146/annurev-arplant-043014-115540 · Cited by 150
The importance of northern peatland expansion to the late-Holocene rise of atmospheric methane
Korhola, A. A., Ruppel, M. M., Seppä, H., Väliranta, M., Virtanen, T. A., & Weckström, J. (2010) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.12.010 · Cited by 141
“In contrast, it has also been suggested that anthropogenic activities, namely rice cultivation and biomass burning, drove much of this increase (Ruddiman, 2003).”
BackgroundLi, X., Dodson, J., Zhou, J., & Zhou, X. (2008) · Quaternary International · doi:10.1016/j.quaint.2008.02.009 · Cited by 129
Early Anthropogenic Transformation of the Danube-Black Sea System
Giosan, L., Coolen, M. J. L., Kaplan, J. O., et al. (2012) · Scientific Reports · doi:10.1038/srep00582 · Cited by 131
Banerjee, S., & Arjaliès, D.-L. (2021) · Organization Theory · doi:10.1177/26317877211036714 · Cited by 126
“The Early Anthropocene hypothesis dates the period to about 8,000 years ago, when farming and agriculture became widespread (Ruddiman, 2003).”
BackgroundEarly rice farming and anomalous methane trends
Ruddiman, W. F., Guo, Z., Zhou, X., Wu, H., & Yu, Y. (2008) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2008.03.007 · Cited by 132
“The rising methane trend of the last 5000 years is anomalous compared to the downward CH4 trends during previous early interglacial intervals (Ruddiman and Thomson, 2001; Ruddiman, 2003, 2007).”
BackgroundInfluentialSelf-citationGan, Y., Liang, C., Campbell, C. A., Zentner, R. P., Lemke, R., Wang, H., & Yang, C. (2012) · European Journal of Agronomy · doi:10.1016/j.eja.2012.07.004 · Cited by 128
The Anthropocene Divide: Obscuring Understanding of Social-Environmental Change
Bauer, A. M., & Ellis, E. C. (2018) · Current Anthropology · doi:10.1086/697198 · Cited by 127
“This correspondence has allowed a growing cadre of climate scientists to convincingly argue that “the anthropogenic greenhouse era began thousands of years ago,” as per Ruddiman’s increasingly well-supported “Early Anthropogenic” hypothesis (Ruddiman 2003).”
BackgroundLand system architecture: Using land systems to adapt and mitigate global environmental change
Turner, B. L., Janetos, A. C., Verburg, P. H., & Murray, A. T. (2013) · Global Environmental Change · doi:10.1016/j.gloenvcha.2012.12.009 · Cited by 127
Fire-free land use in pre-1492 Amazonian savannas
Iriarte, J., Power, M. J., Rostain, S., Mayle, F. E., Jones, H. T., Watling, J. G., Whitney, B. S., & McKey, D. (2012) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1201461109 · Cited by 122
(2019) · Cambridge University Press eBooks · Cited by 125
Can humans force a return to a ‘Cretaceous’ climate?
Hay, W. W. (2010) · Sedimentary Geology · doi:10.1016/j.sedgeo.2010.04.015 · Cited by 124
Holocene agriculture in the Guanzhong Basin in NW China indicated by pollen and charcoal evidence
Li, X., Shang, X., Dodson, J., & Zhou, X. (2009) · The Holocene · doi:10.1177/0959683609345083 · Cited by 128
Carbon and Climate System Coupling on Timescales from the Precambrian to the Anthropocene
Doney, S. C., & SCHIMEL, D. S. (2007) · Annual Review of Environment and Resources · doi:10.1146/annurev.energy.32.041706.124700 · Cited by 127
Wagner, M., Tarasov, P. E., Hosner, D., Fleck, A., Ehrich, R., Chen, X., & Leipe, C. (2012) · Quaternary International · doi:10.1016/j.quaint.2012.06.039 · Cited by 122
Methane Emissions from Large Dams as Renewable Energy Resources: A Developing Nation Perspective
de Lima, I. B. T., Ramos, F. M., Bambace, L. A. W., & Rosa, R. R. (2007) · Mitigation and Adaptation Strategies for Global Change · doi:10.1007/s11027-007-9086-5 · Cited by 123
“In fact, the practice of flooding terrestrial ecosystems might be altering atmospheric CH4 since the past five thousand years (Ruddiman 2003; Ruddiman et al. 2005).”
BackgroundScience for Global Sustainability: Toward a New ParadigmPreprint
Clark, W. C., Crutzen, P. J., & Schellnhuber, H. J. (2005) · SSRN Electronic Journal · doi:10.2139/ssrn.702501 · Cited by 125
Anthropogenic modification of vegetated landscapes in southern China from 6,000 years ago
Cheng, Z., Weng, C., Steinke, S., & Mohtadi, M. (2018) · Nature Geoscience · doi:10.1038/s41561-018-0250-1 · Cited by 119
The Politics of Climate Activism in the UK: A Social Movement Analysis
North, P. (2011) · Environment and Planning A Economy and Space · doi:10.1068/a43534 · Cited by 121
“Why did activists begin to be concerned about anthropogenic climate change when they did given that we now know that humanity has been changing the climate since the dawn of the industrial revolution, if not before (Ruddiman, 2003)?”
BackgroundStocker, B. D., Strassmann, K., & Joos, F. (2011) · Biogeosciences · doi:10.5194/bg-8-69-2011 · Cited by 125
“This has stimulated a debate about the underlying causes and mechanisms (e.g., Inderm̈uhle et al. , 1999; Broecker et al. , 2001; Brovkin et al., 2002; Ruddiman, 2003; Joos et al. , 2004; Elsig et al. , 2009).”
BackgroundInfluentialStyring, A., Ater, M., Hmimsa, Y., Fraser, R., Miller, H., Neef, R., Pearson, J. A., & Bogaard, A. (2016) · The Anthropocene Review · doi:10.1177/2053019616630762 · Cited by 121
“Agriculture has had a major role in shaping landscapes, soils and vegetation, and the beginning of agriculture is one of the candidates for the onset of the Anthropocene (Ruddiman, 2003).”
BackgroundMurphy, D. J. (2007) · doi:10.1093/acprof:oso/9780199207145.001.0001 · Cited by 146
Allen, J. R. M., & Huntley, B. J. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.02.013 · Cited by 120
Blanchet, C., Tjallingii, R., Frank, M., Lorenzen, J., Reitz, A., Brown, K., Feseker, T., & Brückmann, W. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.01.009 · Cited by 119
“However, environmental and hydrological reconstructions have revealed that subtropical regions have drastically changed during the course of the Holocene (Haug et al., 2001; Ruddiman, 2003).”
BackgroundMethane emissions from newly created marshes in the drawdown area of the Three Gorges Reservoir
Chen, H., Wu, Y., Yuan, X., et al. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2009jd012410 · Cited by 118
Archeology and the Anthropocene
Erlandson, J. M., & Braje, T. J. (2013) · Anthropocene · doi:10.1016/j.ancene.2014.05.003 · Cited by 119
Xiao, X., Yao, A., Hillman, A. L., Shen, J., & Haberle, S. G. (2020) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106297 · Cited by 114
Metadata
- Authors
- Ruddiman, W. F.
- Affiliations
- University of Virginia (US)
- Corresponding author
- Ruddiman, William F.
- Venue
- Climatic Change
- Published
- 2003-12
- Volume
- 61
- Issue
- 3
- Pages
- 261-293
- ISSN
- 0165-0009 (ISSN-L)
- 1573-1480
- OpenAlex
- W2139562946
- Semantic Scholar
- 83a526a6d579874795e7852a395c3e44637efead
- Cited by
- 1,658
- References
- 62
- Citations by year
- 2026: 37 · 2025: 97 · 2024: 80 · 2023: 72 · 2022: 62 · 2021: 115 · 2020: 79 · 2019: 102 · 2018: 80 · 2017: 78 · 2016: 58 · 2015: 70 · 2014: 96 · 2013: 87 · 2012: 56
- FWCI
- 39.15
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- Locations
- Climatic Change (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Social Sciences › Archeology › Archaeology and ancient environmental studies
- Keywords
- anthropogenic greenhouse effect, atmospheric CO2, methane, Holocene, ancient agriculture, forest clearing, rice irrigation, Little Ice Age, bubonic plague, farm abandonment, forest regeneration, carbon sequestration, orbital forcing, paleoclimate, Industrial Revolution, global warming
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