id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-55	Bergami, Caterina; Capotondi, Lucilla; Manta, Daniela Salvagio; Sprovieri, Mario; Vigliotti, Luigi	IONIAN SEA SURFACE TEMPERATURE DURING THE SAPROPEL S1 DEPOSITION INFERRED FROM PLANKTONIC FORAMINIFERAL Mg/Ca AND δ18O 	2013	10	.pdf	application/pdf	8216	429	45	Specifically, the δ18O signal of planktonic foraminifera records the combined effects of global ice volume, sea surface temperature, and region- al evaporation/precipitation budgets, while the Mg/Ca ratio of foraminiferal tests mainly depends on the tem- perature of the water in which the foraminifer calcifies, as basically deduced from cultivating work and field studies (e.g., Nürnberg, 1995, 2000; Nürnberg et al., 1996, 2000; Lea et al., 1999; Mashiotta et al., 1999; Elderfield & Ganssen, 2000: Dekens et al., 2002). Foraminiferal Mg/Ca seawater thermometry is a rapidly developing and increasingly widely used tool for palaeoceanographic reconstructions (Nürnberg et al., 1996; Rosenthal et al., 1997; Lea et al., 1999; Elderfield & Ganssen, 2000; Lea at al., 2000; Anand et al., 2003; Barker et al., 2005).	cache/amq-55.pdf	txt/amq-55.txt