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A
Camillo E, Quadros JP, Santarosa ACláudia A, Costa KB, Toledo FAL.  2020.  An abrupt cooling event recorded around 73 kyr in western South Atlantic. Quaternary International. 542:80-87.
Quintela M, Costa PJM, Fatela F, Drago T, Hoska N, Andrade C, Freitas MC.  2016.  The AD 1755 tsunami deposits onshore and offshore of Algarve (south Portugal): Sediment transport interpretations based on the study of Foraminifera assemblages. Quaternary International. 408, Part A:123-138.
Qu B, Sillanpää M, Li C, Kang S, Stubbins A, Yan F, Aho KSue, Zhou F, Raymond PA.  2017.  Aged dissolved organic carbon exported from rivers of the Tibetan Plateau. PLOS ONE. 12(5):e0178166.
Schneider RJ, McNichol AP, von Reden KF, Elder KL, Gagnon AR, Key RM, Quay PD.  1999.  The Antarctic Radiocarbon Storage Ring. 8th International Conference on Accelerator Mass Spectrometry.
Quay P., Sonnerup R., Munro D., Sweeney C..  2017.  Anthropogenic CO2 accumulation and uptake rates in the Pacific Ocean based on changes in the C-13/C-12 of dissolved inorganic carbon. GLOBAL BIOGEOCHEMICAL CYCLES. 31:59-80.
B
Xu Z, Li T, Clift PD, Wan S, Qiu X, Lim D.  2018.  Bathyal records of enhanced silicate erosion and weathering on the exposed Luzon shelf during glacial lowstands and their significance for atmospheric CO2 sink. Chemical Geology. 476:302-315.
C
Miller K.G, Liu C., Browning J.V, Pekar S., Sugarman P., Van Fossen M.C, Mullikin L., Queen D., Feigenson M.D, Aubry M.P et al..  1996.  Cape May site report. 150X and suppl.:59pp.
Shan S, Qi Y, Tian J, Wang X, Luo C, Zhou C, Zhang X-H, Xin Y, Wang Y.  2020.  Carbon cycling in the deep Mariana Trench in the western north Pacific Ocean: Insights from radiocarbon proxy data. Deep Sea Research Part I: Oceanographic Research Papers. 164:103370.
Yao P., Wang X.C, Bianchi T.S, Yang Z.S, Fu L., Zhang X.H, Chen L., Zhao B., Morrison E.S, Shields M.R et al..  2020.  Carbon Cycling in the World's Deepest Blue Hole. Journal of Geophysical Research: Biogeosciences. 125(2)
Shan S, Luo C, Qi Y, Cai W‐J, Sun S, Fan D, Wang X.  2021.  Carbon Isotopic and Lithologic Constraints on the Sources and Cycling of Inorganic Carbon in Four Large Rivers in China: Yangtze, Yellow, Pearl, and Heilongjiang. Journal of Geophysical Research: Biogeosciences. 126(2)
Jingtao Z, Chang F, Li T, Qingyun N, Li Q.  2008.  Carbonate cycle and its control factors in Kuroshio source region during the last 190ka BP. Yanshi Xuebao = Acta Petrologica Sinica. 24(6):1401-1401-1410.
Quay P., Sonnerup R., Westby T., Stutsman J., McNichol A..  2003.  Changes in the 13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic CO2 uptake. Global Biogeochemical Cycles. 17:1-4.
Quay P.D, Sonnerup R., Westby T., Stutsman J., McNichol A.P.  2002.  Changes in the 13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic CO2 uptake. Global Biogeochemical Cycles. 17(1):4-1-4-20.
Quay P.D, Sonnerup T., Westby J., Stutsman J., McNichol A.P.  2003.  Changes of the 13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic C)2 uptake. Global Biogeochemical Cycles. 17(1004)
Li GK, Fischer WW, Lamb MP, A. West J, Zhang T, Galy V, Wang XTony, Li S, Qiu H, Li G et al..  2021.  Coal fly ash is a major carbon flux in the Chang Jiang (Yangtze River) basin. Proceedings of the National Academy of Sciences. 118(21):e1921544118.
Schneider RJ, McNichol AP, von Reden KF, Elder KL, Gagnon AR, Key RM, Quay PD.  1998.  A Correction for Aberrations in the Woods Hole Recombinator. Symposium of North-Eastern Accelerator Personnel. World Scientific. SNEAP 1996:123-128.
Currie L.A, Benner, Jr. B.A, Kessler J.D, Klinedinst D.B, Klouda G.A, Marolf J.V, Slater J.F, Wise S.A, Cachier H., Cary R. et al..  2002.  A Critical Evaluation of Interlaboratory Data on Total, Elemental, and Isotopic Carbon in the Carbonaceous Particle Reference Material, NIST SRM 1649a. J Res Natl Inst Stand Technol. 107(3):279-98.
D
Xu C, Zhang S, Beaver M, Wozniak A, Obeid W, Lin Y, Wade TL, Schwehr KA, Lin P, Sun L et al..  2018.  Decreased sedimentation efficiency of petro- and non-petro-carbon caused by a dispersant for Macondo surrogate oil in a mesocosm simulating a coastal microbial community. Marine Chemistry. 206:34-43.
Qi Y, Fu W, Tian J, Luo C, Shan S, Sun S, Ren P, Zhang H, Liu J, Zhang X et al..  2020.  Dissolved black carbon is not likely a significant refractory organic carbon pool in rivers and oceansAbstract. Nature Communications. 11(1)
E
Ciugudean H, Quinn CP.  2015.  The End of the Wietenberg Culture in the Light of New 14C dates and its Chronological Relation Towards the Noua Culture.. Bronze Age Chronology in the Carpathian Basin.
F
Li C, Chen P, Kang S, Yan F, Tripathee L, Wu G, Qu B, Sillanpää M, Yang D, Dittmar T et al..  2018.  Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence. Journal of Geophysical Research: Atmospheres. 123(11):6248-6258.
I
Sonnerup R.E, Quay P.D, McNichol A.P.  2000.  The Indian Ocean 13C Suess effect. Global Biogeochemical Cycles. 14:903-916.
Qin Z, Storozum M, Liu H, Zhang X, Kidder TR.  2019.  Investigating environmental changes as the driving force of agricultural intensification in the lower reaches of the Yellow River: A case study at the Sanyangzhuang site. Quaternary International. 521:25-34.
O
McNichol AP, Quay PD, Stuart DR, Sonnerup RE, Key RM.  2000.  An Ocean-Wide DIC-13 Data Set. 2000 Ocean Sciences Meeting, San Antonio, TX (USA), 24-28 Jan 2000.
McNichol A.P, Quay P.D, Stuart D.R, Sonnerup R.E, Key R.M.  2000.  An ocean-wide DIC-13 data set. AGU Ocean Sciences Meeting.

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