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Pailler, D., and E. Bard (2002), High frequency palaeoceanographic
changes during the past 140000 yr recorded by the organic matter
in sediments of the Iberian margin, Palaeogeogr. Palaeoclimatol.
Palaeoecol., 181(4), 431
Ruddiman, W. F. (1977), Late Quaternary deposition of ice-rafted
sand in the subpolar North Atlantic (lat 40° to 65°N), Geol. Soc.
Am. Bull., 88, 1813
1827.
Salgueiro, E., A. H. L. Voelker, L. de Abreu, F. Abrantes, H.
Meggers, and G. Wefer (2010), Temperature and productivity
changes off the western Iberian margin during the last 150 ky,
Quat. Sci. Rev., 29(5
-
452.
Peliz, A., J. Dubert, A. M. P. Santos, P. B. Oliveira, and B. Le Cann
(2005), Winter upper ocean circulation in the western Iberian
Basin
-
Fronts, eddies and poleward
flows: An overview, Deep
695.
Sanchez, R. F., and P. Relvas (2003), Spring-summer climatological
circulation in the upper layer in the region of Cape St. Vincent,
southwest Portugal, ICES J. Mar. Sci., 60(6), 1232
-
6), 680
-
646.
Peliz, A., J. Dubert, P. Marchesiello, and A. Teles-Machado (2007),
Surface circulation in the Gulf of Cadiz: Model and mean
Sea Res., Part I, 52(4), 621
-
-
1250.
flow structure, J. Geophys. Res., 112, C11015, doi:10.1029/
2007JC004159.
Penduff, T., A. C. de Verdiere, and B. Barnier (2001), General
circulation and intergyre dynamics in the eastern North Atlantic
from a regional primitive equation model, J. Geophys. Res.,
106(C10), 22,313
S
nchez-Goñi, M. F., and S. P. Harrison (2010), Millennial-scale
climate variability and vegetation changes during the last glacial:
Concepts and terminology, Quat. Sci. Rev., 29(21
á
-
22), 2823
-
2827.
S
nchez-Goñi, M. F., A. Landais, W. J. Fletcher, F. Naughton, S.
Desprat, and J. Duprat (2008), Contrasting impacts of Dansgaard-
Oeschger events over a western European latitudinal transect
modulated by orbital parameters, Quat. Sci. Rev., 27(11
á
22,329.
Perez, F. F., C. G. Castro, X. A. Alvarez-Salgado, and A. F. Rios
(2001), Coupling between the Iberian basin-scale circulation and
the Portugal boundary current system: A chemical study, Deep
Sea Res., Part I, 48(6), 1519
-
-
12),
1151.
Sarnthein, M., et al. (2001), Fundamental modes and abrupt
changes in North Atlantic circulation and climate over the last
60 ky
1136
-
-
1533.
P
aumann, U., J. Duprat, C. Pujol, and L. D. Labeyrie (1996),
SIMMAX: A modern analog technique to deduce Atlantic sea
surface temperatures from planktonic foraminifera in deep-sea
sediments, Paleoceanography, 11(1), 15
Numerical modelling and reconstruction, in The North-
ern North Atlantic: A Changing Environment, edited by P. Schä-
fer et al., pp. 365
-
36.
410, Springer, Heidelberg, Germany.
Saunders, P. M. (1987), Flow through Discovery Gap, J. Phys.
Oceanogr., 17, 631
-
P
aumann, U., et al. (2003), Glacial North Atlantic: Sea-surface
conditions reconstructed by GLAMAP 2000, Paleoceanography,
18(3), 1065, doi:10.1029/2002PA000774.
Pingree, R. D., C. Garcia-Soto, and B. Sinha (1999), Position and
structure of the Subtropical/Azores Front region from combined
Lagrangian and remote sensing (IR/altimeter/SeaWiFS) measure-
ments, J. Mar. Biol. Assoc. U.K., 79(5), 769
643.
Schlitzer, R. (2000), Electronic atlas of WOCE hydrographic and
tracer data now available, Eos Trans. AGU, 81(5), 45.
Schmiedl, G., T. Kuhnt, W. Ehrmann, K.-C. Emeis, Y. Hamann, U.
Kotthoff, P. Dulski, and J. Pross (2010), Climatic forcing of
eastern Mediterranean deep-water formation and benthic ecosys-
tems during the past 22 000 years, Quat. Sci. Rev., 29(23
-
792.
Rashid, H., and E. A. Boyle (2007), Mixed-layer deepening during
Heinrich Events: A multi-planktonic foraminiferal
-
-
24),
18 O ap-
δ
3020.
Schönfeld, J., and R. Zahn (2000), Late Glacial to Holocene history
of the Mediterranean Out
3006
-
441.
Relvas, P., and E. D. Barton (2002), Mesoscale patterns in the Cape
São Vicente (Iberian Peninsula) upwelling region, J. Geophys.
Res., 107(C10), 3164, doi:10.1029/2000JC000456.
Richardson, P. L., A. S. Bower, and W. Zenk (2000), A census of
meddies tracked by
proach, Science, 318(5849), 439
-
ow. Evidence from benthic foraminif-
eral assemblages and stable isotopes at the Portuguese margin,
Palaeogeogr. Palaeoclimatol. Palaeoecol., 159,85
111.
Schönfeld, J., R. Zahn, and L. de Abreu (2003), Surface and deep
water response to rapid climate changes at the western Iberian
margin, Global Planet. Change, 36(4), 237
-
250.
Rios, A. F., F. F. Perez, and F. Fraga (1992), Water masses in the
upper and middle North-Atlantic Ocean east of the Azores, Deep
Sea Res., Part A, 39(3
oats, Progr. Oceanogr., 45, 209
-
264.
Serra, N., and I. Ambar (2002), Eddy generation in the Mediterra-
nean undercurrent, Deep Sea Res., Part II, 49(19), 4225
-
658.
Rogerson, M., E. J. Rohling, P. P. E. Weaver, and J. W. Murray
(2004), The Azores Front since the Last Glacial Maximum, Earth
Planet. Sci. Lett., 222(3
-
4A), 645
-
4243.
Shackleton, N. J., M. A. Hall, and E. Vincent (2000), Phase relation-
ships between millennial-scale events 64,000-24,000 years ago,
Paleoceanography, 15(6), 565
-
789.
Rogerson, M., E. J. Rohling, P. P. E. Weaver, and J. W. Murray
(2005), Glacial to interglacial changes in the settling depth of the
Mediterranean Out
-
4), 779
-
569.
Sierro, F. J., et al. (2005), Impact of iceberg melting on Mediterra-
nean thermohaline circulation during Heinrich events, Paleocea-
nography, 20, PA2019, doi:10.1029/2004PA001051.
Skinner, L. C., and H. Elder
-
ow plume, Paleoceanography, 20, PA3007,
doi:10.1029/2004PA001106.
Roucoux, K. H., L. de Abreu, N. J. Shackleton, and P. C. Tzedakis
(2005), The response of NW Iberian vegetation to North
Atlantic climate oscillations during the last 65 kyr, Quat. Sci.
Rev., 24(14
fluctuations in the
deep North Atlantic heat budget during the last glacial period,
Paleoceanography, 22, PA1205, doi:10.1029/2006PA001338.
Skinner, L. C., and N. J. Shackleton (2004), Rapid transient
changes in northeast Atlantic deep water ventilation age across
eld (2007), Rapid
-
15), 1637
-
1653.
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