E. Bard

Details der Publikationsliste

Zeitraum

1993 - 2008

Anzahl

26

Co-Autoren

Reply to Comment on "The timing and evolution of the post-glacial transgression across the Sea of Marmara shelf south of Istanbul" by Hiscott et al., Marine Geology 248, 228-236 (2008)

ERIS, K. K., RYAN, W. B. F., CAGATAY, M. N., LERICOLAIS, Gilles, SANCAR, U., BARD, E., ...

In their comment Hiscott and co-authors adhere rigidly to ages and sources for sedimentary units in the subsurface of the Marmara shelf that they have previously reported in their publications from...

Sequence Databases (2008)

R Eports, W. S. Broecker, E. Clark, I. Hajdas, G. Bonani, L. Beaufort, ...

advised us that it was not possible to identify milligram-sized fragments of tropical woods; rather, a hand-sized piece of wood would be required. He also commented that, once waterlogged, any wood...

The timing and evolution of the post-glacial transgression across the Sea of Marmara shelf south of Istanbul (2007)

ERIS, K, RYAN, W, CAGATAY, M, SANCAR, U, LERICOLAIS, Gilles, MENOT, G, ...

High-resolution seismic reflection profiles and analyses of the sedimentary substrate at the Sea of Marmara (SoM) entrance to the Strait of Istanbul (Sol, Bosphorus) provide a detailed record of the...

Timing of meltwater pulse 1a and climate responses to meltwater injections (2006)

Stanford, J.D., Rohling, E.J., Hunter, S.H., Roberts, A.P., Rasmussen, S.O., Bard, E., ...

The temporal relationship between meltwater pulse 1a (mwp-1a) and the climate history of the last deglaciation remains a subject of debate. By combining the Greenland Ice Core Project d18O ice core...

Early reactivation of European rivers during the last deglaciation (2006)

Ménot, G., Bard, E., Rostek, F., Weijers, J.W.H., Hopmans, E.C., Schouten, S., ...

During the Last Glacial Maximum, the sea-level lowstand combined with the large extent of the Fennoscandian and British ice sheets led to the funneling of European continental runoff, resulting in...

Sea-level reversal during Termination II (2006)

Siddall, M., Bard, E., Rohling, E.J., Hemleben, C.

The termination of the penultimate glacial period (TII) shows both similarities and differences to the last termination (TI). Both terminations show significant cold reversals in the postglacial...

Reconstruction of temperature in the Central Alps during the past 2000 yr from a y 18 O stalagmite record (2005)

A. Mangini A, C. Spötl B, P. Verdes A, E. Bard

The precisely dated isotopic composition of a stalagmite from Spannagel Cave in the Central Alps is translated into a highly resolved record of temperature at high elevation during the past 2000 yr....

NotCal04—Comparison/Calibration 14C Records 26–50 Cal kyr BP (2004)

Remmele, S., Reimer, R.W., Reimer, P.J., Bronk Ramsey, C., McCormac, F.G., Kromer, B., ...

The radiocarbon calibration curve IntCal04 extends back to 26 cal kyr BP. While several high-resolution records exist beyond this limit, these data sets exhibit discrepancies of up to several...

Interlaboratory comparison study of Mg/Ca and Sr/Ca measurements in planktonic foraminifera for paleoceanographic research (2004)

Rosenthal, Y., Perron-Cashman, S., Lear, C.H., Bard, E., Barker, S., Billups, K., ...

Thirteen laboratories from the USA and Europe participated in an intercomparison study of Mg/Ca and Sr/Ca measurements in foraminifera. The study included five planktonic species from surface...

Le carbone 14 : progrès récents et limitations de la méthode de datation (1998)

Duplessy, J.C., Arnold, M., Bard, E., Cortijo, E., Labeyrie, L., Laj, C., ...

La méthode de datation par le carbone 14 a permis l'établissement d'une échelle chronologique du Quaternaire Supérieur et a contribué à la découverte de phénomènes insoupçonnés comme...

Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge (1996)

Bard, E., Hamelin, B., Arnold, M., Montaggioni, L., Cabioch, Guy, Faure, G., ...

The timing of the last deglaciation is important to our understanding of the dynamics of large ice sheets and their effects on the Earth's surface. Moreover, the disappearance of the glacial ice...