North Atlantic surface ocean warming and salinization in response to middle Eocene greenhouse warming.

Quantitative reconstructions of hydrological change during ancient greenhouse warming events provide valuable insight into warmer-than-modern hydrological cycles but are limited by paleoclimate proxy uncertainties. We present sea surface temperature (SST) records and seawater oxygen isotope (δO) estimates for the Middle Eocene Climatic Optimum (MECO), using coupled carbonate clumped isotope (Δ) and oxygen isotope (δO) data of well-preserved planktonic foraminifera from the North Atlantic Newfoundland Drifts. These indicate a transient ~3°C warming across the MECO, with absolute temperatures generally in accordance with trace element (Mg/Ca)-based SSTs but lower than biomarker-based SSTs for the same interval.

Cenozoic evolution of deep ocean temperature from clumped isotope thermometry.

Characterizing past climate states is crucial for understanding the future consequences of ongoing greenhouse gas emissions. Here, we revisit the benchmark time series for deep ocean temperature across the past 65 million years using clumped isotope thermometry. Our temperature estimates from the deep Atlantic Ocean are overall much warmer compared with oxygen isotope-based reconstructions, highlighting the likely influence of changes in deep ocean pH and/or seawater oxygen isotope composition on classical oxygen isotope records of the Cenozoic.

InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards.

Increased use and improved methodology of carbonate clumped isotope thermometry has greatly enhanced our ability to interrogate a suite of Earth-system processes. However, interlaboratory discrepancies in quantifying carbonate clumped isotope (Δ) measurements persist, and their specific sources remain unclear. To address interlaboratory differences, we first provide consensus values from the clumped isotope community for four carbonate standards relative to heated and equilibrated gases with 1,819 individual analyses from 10 laboratories.

Preparative resolution of the enantiomers of tert-leucine derivatives by simulated moving bed chromatography.

The enantiomers of two different derivatives of tert-leucine were separated by continuous chromatography on chiral stationary phases applying the simulated moving bed technique. About 1 kg of racemic N-carbobenzoxy-tert-leucine was resolved on the cellulose-based phase Chiralcel OD using a mixture of heptane/ethanol and 0.1% of trifluoroacetic acid modifier as the mobile phase, while 520 g of the N-Boc-tert-leucine-benzylester was resolved on the amylose-based phase Chiralpak AD with a mixture of heptane/2-propanol as the mobile phase.

Ca2+ sensitization in idiopathic dilated human myocardium. Differential in vitro effects of (+)-(5-methyl-6-phenyl)-1,3,5,6-tetrahydro-3,6-methano-1,5-benzodiazoci ne-2,4-dione, a novel purely Ca2+sensitizing agent, and (+)-5-(1-(3,4-dimethoxybenzoyl)-1,2,3,4-tetrahydroquinolin-6-yl)-6-meth yl-3, 6-dihydro-2H-1,3,4-thiadiazin-2-one on skinned fibres and isolated ventricular strips.

(+)-(5-Methyl-6-phenyl)-1,3,5,6-tetrahydro-3,6-methano-1, 5-benzodiazocine-2,4-dione (CAS 165755-40-8, CGP 48506) is a novel Ca2+ sensitizing agent devoid of any other positive inotropic mechanism, particularly phosphodiesterase (PDE) III inhibition. 5-(1-(3,4-Dimethoxybenzoyl)-1,2,3,4-tetrahydroquinolin-6-yl)-6-met hyl-3, 6-dihydro-2H-1,3,4-thiadiazin-2-one (CAS 120223-04-3, EMD 53998) is a PDE III inhibitor with a Ca2+ sensitizing activity residing in its (+)-enantiomer, EMD 57033 (CAS 147527-31-9). In skinned fibres and electrically stimulated left ventricular strips from idiopathic dilated human hearts, New York Heart Association (NYHA) class IV, the Ca2+ sensitizing and inotropic effects of the benzodiazocine CGP 48506 and the thiadiazinones EMD 53998 or EMD 57033 were compared.