@article {2514,
	title = {Marine record of Holocene climate, ocean, and cryosphere interactions: Herbert Sound, James Ross Island, Antarctica},
	journal = {Quaternary Science Reviews},
	volume = {129},
	year = {2015},
	month = {Jan-12-2015},
	pages = {239 - 259},
	abstract = {The sediment record offshore James Ross Island, northeast Antarctic Peninsula presents an unparalleled opportunity to directly compare marine and terrestrial climate records spanning the Holocene in maritime Antarctica. An 11 m drill core was collected between Herbert Sound and Croft Bay as part of the SHALDRIL NBP-0502 initiative and produced the southernmost sediment record from the eastern side of the AP. Thirty-eight radiocarbon ages are used to construct an age model of centennial-scale resolution. Multi-proxy records, including magnetic susceptibility, pebble content, particle size, total organic carbon, and diatom assemblages, were interrogated in the context of nearby Holocene-age ice core, lake, and drift records from James Ross Island. Differences in the timing and expression of Holocene events reflect marine controls on tidewater glaciers, such as water mass configurations and sea ice. Glacial behavior mimics ice core paleotemperatures during the Holocene, with the exception of distinct ocean warming events. Herbert Sound was fully occupied by grounded ice during the Last Glacial Maximum, and experienced rapid lift-off, followed by a floating ice phase. The canopy of floating ice receded by 10 {\textpm} 2.4 cal kyr BP, presumably in response to Early Holocene warming. Herbert Sound and Croft Bay fully deglaciated by 7.2 cal kyr BP, when the Mid Holocene Hypsithermal commenced and the sound became open and productive. An extreme peak in productivity \~{}6.1 cal kyr BP indicates an oceanic warming event that is not reflected in atmospheric temperature or lacustrine sediment records. Increase in sea ice cover and ice rafting mark the onset of the Neoglacial \~{}2.5 cal kyr BP, when pronounced atmospheric cooling is documented in the James Ross Island ice core. Our comparison facilitates more holistic understanding of atmosphere-ocean-cryosphere interactions that may aid predictions of glacial response to future warming and sea-level scenarios.},
	keywords = {Antarctic Peninsula, diatoms, Holocene, paleoceanography, paleoclimatology},
	issn = {02773791},
	doi = {10.1016/j.quascirev.2015.09.009},
	url = {https://doi.org/10.1016/j.quascirev.2015.09.009},
	author = {Minzoni, Rebecca Totten and Anderson, John B. and Fernandez, Rodrigo and Wellner, Julia Smith}
}
@article {215,
	title = {Gualas Glacier sedimentary record of climate and environmental change, Golfo Elefantes, Western Patagonia (46.5{\textdegree}S)},
	journal = {The Holocene},
	year = {2011},
	note = {id: 2118},
	abstract = {Gualas Glacier is an outlet glacier of the Northern Patagonian Icefield, one of the largest temperate ice bodies on Earth. Golfo Elefantes, the depositional basin of Gualas Glacier, has a sedimentary record that spans, with some hiatuses, at least the last ~11.3{\textpm}3.0 ka. During this period the gulf remained free of ice, as suggested by the absence of proximal glacimarine sediment and till in the sedimentary section. This implies that the arcuate terminal moraines that occur along the edges of Golfo Elefantes were formed during the waning stages of the local glacial maxima (Late Pleistocene) or the early Holocene. Between ~11.3{\textpm}3.0 ka and ~4.2{\textpm}0.3{\textendash}1.4 ka, the basin received low sediment input consisting of fine-grained sediments in the form of low concentration density currents that filled bathymetric lows. Sediment discharge increased several times in the late Holocene (~},
	doi = {10.1177/0959683611425545},
	url = {http://hol.sagepub.com/content/early/2011/11/22/0959683611425545.abstract},
	author = {Fernandez, Rodrigo and Anderson, John and Bertrand, S{\'e}bastien and Wellner, Julia}
}
