1. Isotopic record in a marine shallow-water core: Imprint of solar centennial cycles in the past 2 millennia
- Author
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G. Cini Castagnoli, Carla Taricco, and Silvia Maria Alessio
- Subjects
Atmospheric Science ,biology ,Oscillation ,Solar cycles ,Aerospace Engineering ,Solar–terrestrial relationships ,Isotopic record ,Climatic variations ,Astronomy and Astrophysics ,Atmospheric sciences ,biology.organism_classification ,Foraminifera ,Waves and shallow water ,Geophysics ,Oceanography ,Centennial ,Space and Planetary Science ,Period (geology) ,Dendrochronology ,General Earth and Planetary Sciences ,Singular spectrum analysis ,Geology ,Globigerinoides - Abstract
The δ 13 C profile of Globigerinoides ruber , measured in the GT90/3 shallow-water Ionian sea core and dated with high precision, is presented and analyzed using the Singular Spectrum Analysis and the Wavelet Transform. This time series covers the period 200–1979 AD, with a resolution of 3.87 years. The δ 13 C of foraminifera depends on the photosynthetic activity of the symbiontic algae living on the shells, strictly related to the illumination of the sea-surface. Both spectral methods, besides an 11-years oscillation in phase with the Schwabe cycle of the solar activity, show the presence of a centennial cycle that is in phase with the amplitude modulation of the sunspot number series in the last 300 years. Moreover, another climatic record, the tree ring δ 13 C of a Japanese cedar covering the time interval 125–1952 AD, shows a similar centennial oscillation and therefore suggests that this climatic variation is global and in phase with the solar activity.
- Published
- 2005