Increased diatom dissolution in Prydz Bay, East Antarctica linked to inception of the Prydz Bay gyre

References

• Armand L., Crosta X., Romero O. & Pichon J-J. 2005. The biogeography of major diatom taxa in Southern Ocean sediments: 1. Sea-ice related species. Palaeogeography, Palaeoclimatology, Palaeoecology 223: 93–126. doi: 10.1016/j.palaeo.2005.02.015
   Web of Science ®Google Scholar
• Barbara L., Crosta X., Massé G. & Ther O. 2010. Deglacial environments in eastern Prydz Bay, East Antarctica. Quaternary Science Reviews 29: 2731–2740. doi: 10.1016/j.quascirev.2010.06.027
   Web of Science ®Google Scholar
• Chase Z., Kohfeld K.E. & Matsumoto K. 2015. Controls on biogenic silica curial in the Southern Ocean. Global Biogeochemical Cycles 29: 1–18. doi:10.1002/2015GB005186
   Web of Science ®Google Scholar
• Crosta X., Denis D. & Ther O. 2008. Sea-ice seasonality during the Holocene, Adélie Land, East Antarctica. Marine Micropaleontology 66: 222–232. doi: 10.1016/j.marmicro.2007.10.001
   Web of Science ®Google Scholar
• DeMaster D. 2002. The accumulation and cycling of biogenic silica in the Southern Ocean: revisiting the marine silica budget. Deep-Sea Research II 49: 3155–3167. doi: 10.1016/S0967-0645(02)00076-0
   Web of Science ®Google Scholar
• Denis D., Crosta X., Barbara L., Massé G., Renssen H. & Ther O. 2010. Sea-ice and wind variability during the Holocene in East Antarctica: insight on middle-high latitude coupling. Quaternary Science Review 29: 3709–3719. doi: 10.1016/j.quascirev.2010.08.007
   Web of Science ®Google Scholar
• Hammer Ø., Harper D.A.T. & Ryan P.D. 2001. PAST: paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4 (1): 9–18.
   Google Scholar
• Hillenbrand C., Kuhn G. & Frederichs T. 2009. Record of a mid-Pleistocene depositional anomaly in West Antarctic continental margin sediments: and indicator for ice-sheet collapse? Quaternary Science Reviews 28: 1147–1159. doi: 10.1016/j.quascirev.2008.12.010
   Web of Science ®Google Scholar
• Khalil K., Rabouille C., Gallinari M., Soetaert K., DeMaster D. & Ragueneau O. 2007. Constraining biogenic silica dissolution in marine sediments: a comparison between diageneitic models and experimental dissolution rates. Marine Chemistry 106: 223–238. doi: 10.1016/j.marchem.2006.12.004
   Web of Science ®Google Scholar
• Konfirst M.A., Kuhn G., Monien D. & Scherer R.P. 2011. Correlation of early Pliocene diatomite to low amplitude Milankovitch cycles in the ANDRILL AND-1B core. Marine Micropaleontology 80: 114–124. doi: 10.1016/j.marmicro.2011.06.005
   Web of Science ®Google Scholar
• Leventer A. 1992. Modern distributions of diatoms in sediments form the George V Coast, Antarctica. Marine Micropaleontology 19: 315–332. doi: 10.1016/0377-8398(92)90036-J
   Web of Science ®Google Scholar
• Leventer A., Domack E., Dunbar R., Pike J., Stickley C., Maddison E., Brachfeld S., Manley P. & McClennen C. 2006. Marine sediment record from the East Antarctic margin reveals dynamics of ice sheet recession. GSA Today 16 (12): 4–10. doi: 10.1130/GSAT01612A.1
   Google Scholar
• Leventer A. & Dunbar R. 1996. Factors influencing the distribution of diatoms and other algae in the Ross Sea. Journal of Geophysical Research 101 (C8): 18489–18500. doi: 10.1029/96JC00204
   Web of Science ®Google Scholar
• Maddison E., Pike J. & Dunbar R. 2012. Seasonally laminated diatom-rich sediments from Dumont d’Urville Trough, East Antarctic margin: Late-Holocene neoglacial sea-ice conditions. The Holocene 22 (8): 857–875. doi: 10.1177/0959683611434223
   Web of Science ®Google Scholar
• Massom R., Harris P., Michael K. & Potter M. 1998. The distribution and formative processes of latent-heat polynyas in East Antarctica. Annals of Glaciology 27: 420–426.
   Web of Science ®Google Scholar
• Pichon J-J., Bareille G., Labracherie M., Labeyrie L., Baudrimont A. & Turon J-L. 1992. Quantification of the biogenic silica dissolution in the southern ocean sediments. Quaternary Research 37: 361–378. doi: 10.1016/0033-5894(92)90073-R
   Web of Science ®Google Scholar
• Pike J., Crosta X., Maddison E., Stickley C., Denis D., Barbara L. & Renssen H. 2009. Observation on the relationship between the Antarctic coastal diatoms Thalassiosira antarctica Comber and Porosira glacialis (Grunow) Jørgensen and sea-ice concentrations during the late quaternary. Marine Micropaleontology 73: 14–25. doi: 10.1016/j.marmicro.2009.06.005
   Web of Science ®Google Scholar
• Ragueneau O., Tréguer P., Leynaert A., Anderson R., Brzezinski M., DeMaster D., Dugdale R., Dymond J., Fischer G., François R., Heinze C., Maier-Reimer E., Martin-Jézéquel V., Nelson D. & Quéguiner B. 2000. A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy. Global and Planetary Change 26: 317–365. doi: 10.1016/S0921-8181(00)00052-7
   Web of Science ®Google Scholar
• Rathburn A.E., Pichon J.J., Ayress M.A. & DeDeckker P. 1997. Microfossil and stable-isotope evidence for changes in Late Holocene paleoproductivity and paleoceanographic conditions in the Prydz Bay region of Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology. 131: 485–510. doi: 10.1016/S0031-0182(97)00017-5
   Web of Science ®Google Scholar
• Ryves D., Battarbee R. & Fritz S. 2009. The dilemma of disappearing diatoms: incorporating diatom dissolution data into paleoenvironmental modeling and reconstruction. Quaternary Science Reviews 28: 120–136. doi: 10.1016/j.quascirev.2008.08.021
   Web of Science ®Google Scholar
• Shemesh A., Burckle L. & Froelich P. 1989. Dissolution and preservation of Antarctic diatoms and the effect on sediment thanatocoenoses. Quaternary Research 31: 288–308. doi: 10.1016/0033-5894(89)90010-0
   Web of Science ®Google Scholar
• Shimada C., Hasegawa S., Tanimura Y. & Burckle L. 2003. A new index to quantify diatom dissolution levels based on a ratio of Neodenticula seminae frustule components. Micropaleontology 49 (3): 267–276. doi: 10.2113/49.3.267
   Web of Science ®Google Scholar
• Smith N. & Tréguer P. 1994. Physical and chemical oceanography in the vicinity of Prydz bay, Antarctica. In: Southern ocean ecology: the BIOMASS perspective (Ed. by S.Z. El-Sayed), pp. 25–45. Cambridge University Press, Cambridge.
   Google Scholar
• Stickley C., Pike J., Leventer A., Dunbar R., Domack E., Brachfeld S., Manley P. & McClennan C. 2005. Deglacial ocean and climate seasonality in laminated diatom sediments, Mac.Robertson Shelf, Antarctica. Paleogeography, Paleoclimatology, and Paleoecology 227 (4): 290–310. doi: 10.1016/j.palaeo.2005.05.021
   Web of Science ®Google Scholar
• Tamura T., Oshima K. & Niahshi S. 2008. Mapping of sea-ice production for Antarctic coastal polynyas. Geophysical Research Letters 35: L07606. 1.1029/2007GL032903 doi: 10.1029/2007GL032903
   Web of Science ®Google Scholar
• Warnock J.P. & Scherer R.P. 2015. Diatom species abundance and morphologically-based dissolution proxies in coastal Southern Ocean assemblages. Continental Shelf Research 102: 1–8. doi: 10.1016/j.csr.2015.04.012
   Web of Science ®Google Scholar
• Warnock J.P., Scherer R.P. & Loubere P. 2007. A quantitative assessment of diatom dissolution and late quaternary primary productivity in the Eastern Equatorial Pacific. Deep-Sea Research II 54: 772–783. doi: 10.1016/j.dsr2.2007.01.011
   Web of Science ®Google Scholar
• Warnock J.P., Scherer R.P. & Konfirst M.A. 2015. A record of Pleistocene diatom preservation from the Amundsen Sea, West Antarctica with possible implications on silica leakage. Marine Micropaleontology 117: 40–46. doi: 10.1016/j.marmicro.2015.04.001
   Web of Science ®Google Scholar