Cenozoic mean greenhouse gases and temperature changes with reference to the Anthropocene

• Published in: Global Change Biology
• Main Author: Glikson, Andrew
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2016
• Subjects: ice core
• Online Access: http://dx.doi.org/10.1111/gcb.13342; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13342; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13342

Abstract Cenozoic greenhouse gases ( GHG ) variations and warming periods underscore the extreme rates of current climate change, with major implications for the adaptability and survivability of terrestrial and marine habitats. Current rise rate of greenhouse gases, reaching 3.3 ppm CO 2 per year during March 2015–2016, is the fastest recorded since the Paleocene‐Eocene Thermal Event ( PETM ) when carbon release to the atmosphere was about an order of magnitude less than at present. The ice core evidence of concentration of ( GHG ) and temperatures in the atmosphere/ocean/cryosphere system over the last 740 kyr suggests that the rate of rise in GHG over the last ~260 years, CO 2 rates rising from 0.94 ppm yr −1 in 1959 (315.97 ppm) to 1.62 ppm yr −1 in 2000 (369.52 ppm) to 3.05 ppm yr −1 in 2015 (400.83 ppm), constitutes a unique spike in the history of the atmosphere. The reliance of pre‐740 kyr paleoclimate estimates on multiple proxies, including benthic and plankton fossils, fossil plants, residual organic matter, major and trace elements in fossils, sediments and soils, place limits on the resolution of pre‐upper Pleistocene paleoclimate estimates, rendering it likely recorded mean Cenozoic paleoclimate trends may conceal abrupt short‐term climate fluctuations. However, as exemplified by the Paleocene–Eocene thermal maximum ( PETM ) and earlier GHG and temperature spikes associated with major volcanic and asteroid impact events, the long‐term residence time of CO 2 in the atmosphere extends the signatures of abrupt warming events to within detection limits of multiple paleoproxies. The mean post‐1750 temperature rise rate (approximately ~0.0034 °C per yr, or ~0.008 °C per yr where temperature is not masked by sulfur aerosols) exceeds those of the PETM (approximately ~0.0008–0.0015 °C per yr) by an order of magnitude and mean glacial termination warming rates (last glacial termination [ LGT ] ~ 0.00039; Eemian ~0.0004 °C per yr) by near to an order of magnitude. Consistent with previous interglacial peaks ...