Diploptene <i>δ</i>¹³C values from contemporary thermokarst lake sediments show complex spatial variation

A key feature of the continuous culture chemostat relevant to our study is that at this steady-state, the constant dilution rate of the reactor (the medium flow rate divided by

Big Delta values between the samples and the laboratory standards are also determined for daily measurements, which are used to anchor the individual measurements on the pri- mary

The comparison with the results of multi-channel singular-spectrum analysis (MSSA) applied to a data set of 26 Northern Hemisphere (NH) temperature-proxy records shows that

in the vegetation using the measured δ 13 C of paleosol organic matter without or with a correction for isotopic enrichment due to soil organic matter decomposition. Here we use

This may be a consequence of the very high sea-ice di ff usivities (SID) that have been allowed in the ensemble leading to increased brine rejection and AABW production. + 0.83 in

Thus, a new mixing line (HH2-E mixing line) was re-calculated between the sampling location after the floodgate and estuarine water (Fig.. However, the DIN and isotopic trends did

Hence if reaction ( 1 ) is the primary removal process for methane we would expect smooth seasonal cycles in the mixing ratio of methane following those of OH with a phase shift of

The whole discussion about the inadequacy of hydrological models we have witnessed of late, is related to the wrong concept of what a model is.. Good models