Calibration of the carbon isotope composition (δ¹³C) of benthic foraminifera

This result could be attributed to three factors: first, for some causes, subcause structure is different by age, and each subcause is differentially impacted by production

Yutin N, Suzuki MT, Teeling H, Weber M, Venter JC, Rusch DB & Béjà O (2007) Assessing diversity and biogeography of aerobic anoxygenic phototrophic bacteria in surface waters

In this thesis, the development of the catalytic cyanoacylation of carbonyl compounds, and the synthesis of a new class of chiral stannacyclohexane catalysts are

L’ouverture des archives au public scientifique décidée par Léon XIII ne modifia pas non plus cette attitude et si les entreprises éditoriales consacrées aux XVIe et XVIIe

Winter mixed layers observations are rather scarce in the Western Nansen Basin. In particular, favorable comparisons with A ‐ TWAIN mooring time series of deep winter mixed layers

subtle climatic variations can be recorded through stable carbon isotope ratios of oak 392. charcoals, whereas this was not the case for latewood proportion (see

Figure 9 shows the horizontal structure of the mean flow obtained in the different runs at 2,000 m depth, as well as the vertical structure at a section located near the center of

Measured and derived water isotope time series are identified using the paleo- Data_variableType and paleoData_description fields and should not be confused with the