@article {2711,
	title = {Interstadial Rise and Younger Dryas Demise of Scotland{\textquoteright}s Last Ice Fields},
	journal = {Paleoceanography and Paleoclimatology},
	volume = {33},
	year = {2018},
	month = {Jan-04-2018},
	pages = {412 - 429},
	abstract = {Establishing the atmospheric expression of abrupt climate change during the last glacial termination is key to understanding driving mechanisms. In this paper, we present a new 14C chronology of glacier behavior during late-glacial time from the Scottish Highlands, located close to the overturning region of the North Atlantic Ocean. Our results indicate that the last pulse of glaciation culminated between ~12.8 and ~12.6 ka, during the earliest part of the Younger Dryas stadial and as much as a millennium earlier than several recent estimates. Comparison of our results with existing minimum-limiting 14C data also suggests that the subsequent deglaciation of Scotland was rapid and occurred during full stadial conditions in the North Atlantic. We attribute this pattern of ice recession to enhanced summertime melting, despite severely cool winters, and propose that relatively warm summers are a fundamental characteristic of North Atlantic stadials.},
	keywords = {late glacial, Loch Lomond Readvance, marine reservoir effect, moraine chronology, radiocarbon, seasonality},
	doi = {10.1002/palo.v33.410.1002/2018PA003341},
	url = {https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2018PA003341},
	author = {Bromley, G. and Putnam, A. and Borns, H. and Lowell, T. and Sandford, T. and Barrell, D.}
}
@article {2440,
	title = {Constant Holocene Southern-Ocean 14C reservoir ages and ice-shelf flow rates},
	volume = {296},
	year = {2010},
	month = {2010/7/15/},
	pages = {115 - 123},
	abstract = {Southern Ocean radiocarbon reservoir ages (i.e. non-zero radiocarbon ages in seawater) are the highest in the world{\textquoteright}s surface ocean. Constraining these reservoir ages at present and in the past is important not only because unknown reservoir ages limit the interpretation of Antarctic radiocarbon chronologies, but also because reservoir ages provide information about ocean circulation (as a recorder of past circulation and as an end member for major deep-water masses in today{\textquoteright}s ocean). In this study, we use paired U/Th and 14C ages of an unusual set of solitary coral samples trapped by fringing ice shelves in the Ross Sea to provide the first detailed study of Holocene reservoir ages for the Southern Ocean. Our results indicate a relatively constant marine radiocarbon reservoir age of 1144 {\textpm} 120 years for the past 6000 years. These results are consistent with extrapolation of the relationship between 14C and alkalinity seen elsewhere, supporting the use of this empirical relationship in high latitudes. The results also suggest constant deep-ocean circulation and air{\textendash}sea exchange during the Holocene and provide a good target for tuning ocean models of modern circulation. Combining the new ages for corals with their distance from the modern-day ice-shelf grounding line provides some of the first long-term records of ice-shelf velocities for any region and indicates constant flow of the McMurdo Ice Shelf during the Holocene, at a rate similar to that observed today.},
	keywords = {coral, marine reservoir effect, McMurdo Ice Shelf, radiocarbon, Southern Ocean, U/Th dating},
	isbn = {0012-821X},
	doi = {10.1016/j.epsl.2010.04.054},
	url = {http://www.sciencedirect.com/science/article/pii/S0012821X10003067},
	author = {Hall, Brenda L. and Henderson, Gideon M. and Baroni, Carlo and Kellogg, Thomas B.}
}
@article { ISI:000279905800011,
	title = {Constant Holocene Southern-Ocean C-14 reservoir ages and ice-shelf flow rates},
	journal = {EARTH AND PLANETARY SCIENCE LETTERS},
	volume = {296},
	number = {{1-2}},
	year = {2010},
	month = {JUL 15},
	pages = {115-123},
	type = {Article},
	abstract = {Southern Ocean radiocarbon reservoir ages (i.e. non-zero radiocarbon ages in seawater) are the highest in the world{\textquoteright}s surface ocean. Constraining these reservoir ages at present and in the past is important not only because unknown reservoir ages limit the interpretation of Antarctic radiocarbon chronologies, but also because reservoir ages provide information about ocean circulation (as a recorder of past circulation and as an end member for major deep-water masses in today{\textquoteright}s ocean). In this study, we use paired U/Th and C-14 ages of an unusual set of solitary coral samples trapped by fringing ice shelves in the Ross Sea to provide the first detailed study of Holocene reservoir ages for the Southern Ocean. Our results indicate a relatively constant marine radiocarbon reservoir age of 1144 +/- 120 years for the past 6000 years. These results are consistent with extrapolation of the relationship between C-14 and alkalinity seen elsewhere, supporting the use of this empirical relationship in high latitudes. The results also suggest constant deep-ocean circulation and air-sea exchange during the Holocene and provide a good target for tuning ocean models of modern circulation. Combining the new ages for corals with their distance from the modern-day ice-shelf grounding line provides some of the first long-term records of ice-shelf velocities for any region and indicates constant flow of the McMurdo Ice Shelf during the Holocene, at a rate similar to that observed today. (C) 2010 Elsevier B.V. All rights reserved.},
	keywords = {coral, marine reservoir effect, McMurdo Ice Shelf, radiocarbon, Southern Ocean, U/Th dating},
	issn = {0012-821X},
	doi = {10.1016/j.epsl.2010.04.054},
	author = {Hall, Brenda L. and Henderson, Gideon M. and Baroni, Carlo and Kellogg, Thomas B.}
}
