@article {69,
	title = {Holocene sea-surface temperature variability in the Chilean fjord region},
	journal = {Quaternary Research},
	volume = {82},
	year = {2014},
	pages = {342-353},
	abstract = {Here we provide three new Holocene (11{\textendash}0 cal ka BP) alkenone-derived sea surface temperature (SST) records from the southernmost Chilean fjord region (50{\textendash}53{\textdegree}S). SST estimates may be biased towards summer temperature in this region, as revealed by a large set of surface sediments. The Holocene records show consistently warmer than present-day SSTs except for the past ~ 0.6 cal ka BP. However, they do not exhibit an early Holocene temperature optimum as registered further north off Chile and in Antarctica. This may have resulted from a combination of factors including decreased inflow of warmer open marine waters due to lower sea-level stands, enhanced advection of colder and fresher inner fjord waters, and stronger westerly winds. During the mid-Holocene, pronounced short-term variations of up to 2.5{\textdegree}C and a cooling centered at ~ 5 cal ka BP, which coincides with the first Neoglacial glacier advance in the Southern Andes, are recorded. The latest Holocene is characterized by two pronounced cold events centered at ~ 0.6 and 0.25 cal ka BP, i.e., during the Little Ice Age. These cold events have lower amplitudes in the offshore records, suggesting an amplification of the SST signal in the inner fjords.},
	issn = {0033-5894},
	doi = {10.1016/j.yqres.2014.07.009},
	url = {http://www.sciencedirect.com/science/article/pii/S0033589414000933},
	author = {Caniup{\'a}n, Magaly and Lamy, Frank and Lange, Carina B. and Kaiser, J{\'e}r{\^o}me and Kilian, Rolf and Arz, Helge W. and Le{\'o}n, Tania and Mollenhauer, Gesine and Sandoval, Susana and De Pol-Holz, Ricardo and Pantoja, Silvio and Wellner, Julia and Tiedemann, Ralf}
}
@article {2566,
	title = {Sea surface temperature variability and sea-ice extent in the subarctic northwest Pacific during the past 15,000 years},
	journal = {Paleoceanography},
	volume = {27},
	year = {2012},
	month = {Jan-09-2012},
	pages = {n/a - n/a},
	abstract = {Past changes in North Pacific sea surface temperatures and sea-ice conditions are proposed to play a crucial role in deglacial climate development and ocean circulation but are less well known than from the North Atlantic. Here, we present new alkenone-based sea surface temperature records from the subarctic northwest Pacific and its marginal seas (Bering Sea and Sea of Okhotsk) for the time interval of the last 15 kyr, indicating millennial-scale sea surface temperature fluctuations similar to short-term deglacial climate oscillations known from Greenland ice core records. Past changes in sea-ice distribution are derived from relative percentage of specific diatom groups and qualitative assessment of the IP25biomarker related to sea-ice diatoms. The deglacial variability in sea-ice extent matches the sea surface temperature fluctuations. These fluctuations suggest a linkage to deglacial variations in Atlantic meridional overturning circulation and a close atmospheric coupling between the North Pacific and North Atlantic. During the Holocene the subarctic North Pacific is marked by complex sea surface temperature trends, which do not support the hypothesis of a Holocene seesaw in temperature development between the North Atlantic and the North Pacific.},
	doi = {10.1029/2012PA002292},
	url = {http://doi.wiley.com/10.1029/2012PA002292},
	author = {Max, Lars and Riethdorf, Jan-Rainer and Tiedemann, Ralf and Smirnova, Maria and Lembke-Jene, Lester and Fahl, Kirsten and {\"u}rnberg, Dirk and Matul, Alexander and Mollenhauer, Gesine}
}
