Search Results - (Author, Cooperation:E. Bard)
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1Staff View
Publication Date: 2013-11-16Publisher: American Association for the Advancement of Science (AAAS)Print ISSN: 0036-8075Electronic ISSN: 1095-9203Topics: BiologyChemistry and PharmacologyComputer ScienceMedicineNatural Sciences in GeneralPhysicsKeywords: *Climate Change ; *Humidity ; *Ice Cover ; *Tropical ClimatePublished by: -
2J. D. Shakun ; P. U. Clark ; F. He ; S. A. Marcott ; A. C. Mix ; Z. Liu ; B. Otto-Bliesner ; A. Schmittner ; E. Bard
Nature Publishing Group (NPG)
Published 2012Staff ViewPublication Date: 2012-04-07Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsKeywords: Antarctic Regions ; Atmosphere/chemistry ; Carbon Dioxide/*analysis ; Fossils ; Geography ; Geologic Sediments/chemistry ; Global Warming/*statistics & numerical data ; Greenland ; History, Ancient ; *Ice Cover ; Models, Theoretical ; Monte Carlo Method ; Pollen ; Seawater/analysis ; *Temperature ; UncertaintyPublished by: -
3P. Deschamps ; N. Durand ; E. Bard ; B. Hamelin ; G. Camoin ; A. L. Thomas ; G. M. Henderson ; J. Okuno ; Y. Yokoyama
Nature Publishing Group (NPG)
Published 2012Staff ViewPublication Date: 2012-03-31Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsKeywords: Animals ; Anthozoa ; Coral Reefs ; Freezing ; Global Warming/*history ; History, Ancient ; *Ice Cover ; Oceans and Seas ; Polynesia ; Seawater/*analysis ; Time Factors ; UncertaintyPublished by: -
4Bard, E. ; Arnold, M. ; Ostlund, H.G. ; Maurice, P. ; Monfray, P. ; Duplessy, J.-C.
Amsterdam : ElsevierStaff ViewISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
5Staff View
ISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
6Bard, E. ; Arnold, M. ; Mangerud, J. ; Paterne, M. ; Labeyrie, L. ; Duprat, J. ; Melieres, M.-A. ; Sonstegaard, E. ; Duplessy, J.-C.
Amsterdam : ElsevierStaff ViewISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
7Duplessy, J.C. ; Bard, E. ; Arnold, M. ; Shackleton, N.J. ; Duprat, J. ; Labeyrie, L.
Amsterdam : ElsevierStaff ViewISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
8Bard, E. ; Hamelin, B. ; Fairbanks, R.G. ; Zindler, A. ; Mathieu, G. ; Arnold, M.
Amsterdam : ElsevierStaff ViewISSN: 0168-583XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: PhysicsType of Medium: Electronic ResourceURL: -
9Staff View
ISSN: 0168-583XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: PhysicsType of Medium: Electronic ResourceURL: -
10Staff View
ISSN: 0168-583XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: PhysicsType of Medium: Electronic ResourceURL: -
11Staff View
ISSN: 0168-583XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: PhysicsType of Medium: Electronic ResourceURL: -
12Staff View
ISSN: 0022-197XTopics: Political ScienceURL: -
13Staff View
ISSN: 1432-0894Source: Springer Online Journal Archives 1860-2000Topics: GeosciencesPhysicsNotes: Abstract Bioturbation acts as a low-pass filter in displacing and reducing the amplitudes of stratigraphic signals. This often leads to a loss of high-frequency events in the stratigraphic record. In addition, when considering an isotopic signal δ18O,14C measured in stratigraphic “carriers”, such as foraminifera, bioturbation and carrier abundance changes can create artifacts which may be falsely interpreted as leads or lags in the paleoclimatic record. We presenthere a model in which bioturbationis treated as a time-invariant filter whose impulse response function (IRF) is like that of a first-order system. The method involves first deconvoluting the abundance curves of the carriers and then the isotopic signals using the restored “carrier” abundances. This analysis was initially used to artificially generate ideal curves, with the aim of qualitatively modelling the effects of bioturbation. Following this, deconvolved curves were obtained using data from the core CH73-139C using δ18O, A. M. S. C-14 ages, and abundances of two planktonic foraminifera:G. bulloides andN. pachyderma left-coiling. A comparison of the data with the unmixed curves enables separation of the bioturbation artifacts and the construction of a common deglaciation curve based on the restored signals. Importantly, the model emphasizes some severe limitations of mathematical analysis of stratigraphic signals.Type of Medium: Electronic ResourceURL: