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A detailed radiostratigraphic data set for the central East Antarctic Plateau spanning from the Holocene to the mid-Pleistocene Earth Systems Science Data, 2021 (Ref: 16545)
Authors:
Cavitte M.G.P.Young D.A.Mulvaney R.Ritz C.Roberts J.L.
Category 1: Peer-reviewed literature

Improved estimates of preindustrial biomass burning reduce the magnitude of aerosol climate forcing in the Southern Hemisphere Science Advances, 2021 (Ref: 16416)
Authors:
Liu P.Kaplan J.O.Mickley L.J.Li Y.Chellman N.J.Arienzo M.M.Kodros J.K.Pierce J.R.Sigl M.Freitag J.Mulvaney R.Curran M. A. J.McConnel J.R.
Category 1: Peer-reviewed literature

Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake Nature Geoscience, 2016 (Ref: 15781)
Authors:
Rubino M.Etheridge D.M.Trudinger C.M.Allison C.E.Rayner P.J.Enting I.Mulvaney R.Steele L.P.Langenfelds R.L.Sturges W.T.Curran M.A.J.Smith A.M.
Category 1: Peer-reviewed literature

Atmospheric CO2 and delta13C-CO2 reconstruction of the Little Ice Age from Antarctic ice cores Geophysical Research Abstracts, European Geosciences Union (EGU) General Assembly 2015, Vienna, Austria, 12-17 April 2015, 2015 (Ref: 15720)
Authors:
Rubino M.Etheridge D.Trudinger C.Allison C.Mulvaney R.Steele P.Langenfeld R.Sturges W.T.Curran M.Smith A.
Category 3: Verbal presentation

The decrease of atmospheric CO2 concentration recorded in Antarctic ice around 1600 AD is one of the mostsignificant atmospheric changes to have occurred during the last millennia, before the onset of the industrial period.Together with the temperature decrease…

A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum Quaternary Science Reviews, 2014 (Ref: 15428)
Authors:
The RAISED Consortium Bentley M.J.Cofaigh C.Ó. Anderson J.B.Conway H.Davies B.Graham A.G.C.Hillenbrand C.-D. Hodgson D.A.Jamieson S.S.R.Larter R.D.Mackintosh A.Smith J.A.Verleyen E.Ackert R.P.Bart P.J.Berg S.Brunstein D.Canals M.Colhoun E.A.Crosta X.Dickens W.A.Domack E.Dowdeswell J.A.Dunbar R.Ehrmann W.Evans J.Favier V.Fink D.Fogwill C.J.Glasser N.F.Gohl K.Golledge N.R.Goodwin I.Gore D.B.Greenwood S.L.Hall B.L.Hall K.Hedding D.W.Hein A.S.Hocking E.P.Jakobsson M.Johnson J.S.Jomelli V.Selwyn Jones R.Klages J.P.Kristoffersen Y.Kuhn G.Leventer A.Licht K.Lilly K.Lindow J.Livingstone S.J.Massé G.McGlone M.S.McKay R.M.Melles M.Miura H.Mulvaney R.Nel W.Nitsche F.O.O'Brien P.E.Post A.L.Roberts S.J.Saunders K.M.Selkirk P.M.Simms A.R.Spiegel C.Stolldorf T.D.Sugden D.E.van der Putten N.van Ommen T.D.Verfaillie D.Vyverman W.Wagner B.White D.A.Witus A.E.Zwartz D.
Category 1: Peer-reviewed literature

Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core. Climate of the Past, 2013 (Ref: 15216)
Authors:
Fischer H.Severinghaus J.Brook E.Wolff E.Albert M.Alemany O.Arthern R.Bentley C.Blankenship D.Chappellaz J.Creyts T.Dahl-Jensen D.Dinn M.Frezzotti M.Fujita S.Gallee H.Hindmarsh R.Hudspeth D.Jugie G Kawamura K.Lipenkov V.Miller H.Mulvaney R.Parrenin F.Pattyn E.Ritz C.Schwander J.Steinhage D.van Ommen T.D.Wilhelms F.
Category 1: Peer-reviewed literature

Antarctic climate and environment history in the pre-instrumental period. Antarctic Climate Change and the Environment, 2009 (Ref: 13973)
Authors:
Abram N.Anderson J.Bargelloni L.Barrett P.Bentley M.J.Bertler N.A.N.Chown S.Clarke A.Convey P.Crame A.Crosta X.Curran M.di Prisco G.Francis J.E.Goodwin I.Gutt J.Hodgson D.A.Masse G.Masson-Delmotte V.Mayewski P.A.Mulvaney R.Peck L.Portner H-O. Rothlisberger R.Stevens M.I.Summerhayes C.P.van Ommen T.Verde C.Verleyen E.Vyverman W.Wiencke C.Zane L.
Category 1: Peer-reviewed literature

Continental-scale temperature variability during the past two millennia. Nature Geoscience: Progress Article, 2013 (Ref: 15037)
Authors:
Ahmed M.Anchukaitis K.J.Asrat A.Borgaonkar H.P.Braida M.Buckley B.M.Büntgen B.Chase B.M.Christie D.A.Cook E.R.Curran M.A.J.Diaz H.F.Esper J.Fan Z.-X. Gaire N.P.Ge Q.Gergis J.González-Rouco J.F.Goosse H.Grab S.W.Graham N.Graham R.Grosjean M.Hanhijärvi S.T.Kaufman D.S.Kiefer T.Kimura K.Korhola A.A.Krusic P.J.Lara A.Lézine A.-M. Ljungqvist F.C.Lorrey A.M.Luterbacher J.Masson-Delmotte V.McCarroll D.McConnell J.R.McKay N.P.Morales M.S.Moy A.D.Mulvaney R.Mundo I.A.Nakatsuka T.Nash D.J.Neukom R.Nicholson S.E.Oerter H.Palmer J.G.Phipps S.J.Prieto M.R.Rivera A.Sano M.Severi M.Shanahan T.M.Shao X.Shi F.Sigl M.Smerdon J.E.Solomina O.N.Steig E.J.Stenni B.Thamban M.Trouet V.Turney C.S.M.Umer M.van Ommen T.D.Verschuren D.Viau A.E.Villalba R.Vinther B.M.von Gunten L.Wagner S.Wahl E.R.Wanner H.Werner J.P.White J.W.C.Yasue K.Zorita E.
Category 1: Peer-reviewed literature

Developing an ice core reconstruction of regional sea ice changes around Antarctica Geochimica et Cosmochimica Acta, 2008 (Ref: 13697)
Authors:
Abram N.J.McConnell J.Thomas E.R.Curran M.A.J.Mulvaney R.
Category 3: Abstract

Sea ice is a critical but poorly understood component of … Earth’s climate system. A rapid decline in Arctic sea ice over … recent decades has been documented using historical ship … charts and satellite images. However…

The preservation of methanesulphonic acid in frozen ice-core samples Journal of Glaciology, 2008 (Ref: 13695)
Authors:
Abram N.J.Curran M.A.J.Mulvaney R.Vance T.
Category 1: Peer-reviewed literature

Ice-core records of methanesulphonic acid (MSA) provide a potentially powerful tool for … producing proxy records of sea ice, a critical but poorly understood component of the Earth’s climate … system. However, MSA is able to diffuse through solid ice…

The International Trans-Antarctic Scientific Expedition (ITASE): an overview Annals of Glaciology, 2005 (Ref: 12352)
Authors:
Mayewski P.A.Frezzotti M.Bertler N.Van Ommen T.Hamilton G.Jacka T.H.Welch B.Frey M.Qin D.Ren J.Simões J.Fily M.Oerter H.Nishio F.Isaksson E.Mulvaney R.Holmund P.Lipenkov V.Goodwin I.
Category 1: Peer-reviewed literature

From its original formulation in 1990 the International Trans-Antarctic Scientific Expedition … (ITASE) has had as its primary aim the collection and interpretation of a continent-wide array of … environmental parameters assembled through the coordinated efforts of scientists from several nations.

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