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Monsoon-influenced variations in productivity and lithogenic flux along offshore Saurashtra, NE Arabian Sea during the Holocene and Younger Dryas: A multi-proxy approach [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017-01-01, 483
Azharuddin S.;  Govil P.;  Singh A.D.;  Mishra R.;  Agrawal S.;  Tiwari A.K.;  Kumar K.
View/Download:40/0
 
Fluctuations of Mediterranean Outflow Water circulation in the Gulf of Cadiz during MIS 5 to 7: Evidence from benthic foraminiferal assemblage and stable isotope records [期刊论文]
Global and Planetary Change, 2015-01-01, 133
Singh A.D.;  Rai A.K.;  Tiwari M.;  Naidu P.D.;  Verma K.;  Chaturvedi M.;  Niyogi A.;  Pandey D.
View/Download:34/0
 
A reference time scale for Site U1385 (Shackleton Site) on the SW Iberian Margin [期刊论文]
Global and Planetary Change, 2015-01-01, 133
Hodell D.;  Lourens L.;  Crowhurst S.;  Konijnendijk T.;  Tjallingii R.;  Jiménez-Espejo F.;  Skinner L.;  Tzedakis P.C.;  Abrantes F.;  Acton G.D.;  Zarikian C.A.A.;  Bahr A.;  Balestra B.;  Barranco E.L.;  Carrara G.;  Ducassou E.;  Flood R.D.;  José-Abel Flores;  Furota S.;  Grimalt J.;  Grunert P.;  Hernández-Molina J.;  Kim J.K.;  Krissek L.A.;  Kuroda J.;  Li B.;  Lofi J.;  Margari V.;  Martrat B.;  Miller M.D.;  Nanayama F.;  Nishida N.;  Richter C.;  Rodrigues T.;  Rodríguez-Tovar F.J.;  Roque A.C.F.;  Goñi M.F.S.;  Sierro F.J.;  Singh A.D.;  Sloss C.R.;  Stow D.A.V.;  Takashimizu Y.;  Tzanova A.;  Voelker A.;  Xuan C.;  Williams T.
View/Download:54/0
 
Planktic foraminiferal responses to orbital scale oceanographic changes off the western Iberian margin over the last 900kyr: Results from IODP site U1391 [期刊论文]
Global and Planetary Change, 2015-01-01, 135
Singh A.D.;  Verma K.;  Jaiswal S.;  Alonso-Garcia M.;  Li B.;  Abrantes F.
View/Download:25/0
 
Monsoonal dynamics and evolution of the primary productivity in the eastern Arabian Sea over the past 30 ka [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2014-01-01, 411
Cabarcos E.;  Flores J.A.;  Singh A.D.;  Sierro F.J.
View/Download:16/0
 

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