The clumped isotope (Δ47) proxy is a promising geochemical tool to reconstruct past ocean temperatures far back in time and in unknown settings, due to its unique thermodynamic basis that renders it independent from other environmental factors like seawater composition. Although previously hampered by large sample-size requirements, recent methodological advances have made the paleoceanographic application of Δ47 on small (<5 mg) foraminifer samples possible. Previous studies show a reasonable match between Δ47 calibrations based on synthetic carbonate and various species of planktonic foraminifers. However, studies performed before recent methodological advances were based on relatively few species and data treatment that is now outdate...
The reliable determination of past seawater temperature is fundamental to paleoclimate studies. We t...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
The clumped isotope (Δ47) proxy is a promising geochemical tool to reconstruct past ocean temperatur...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
Applying the clumped isotope (Δ47) thermometer to foraminifer microfossils offers the potential to s...
The reconstruction of past ocean temperatures is fundamental to the study of past climate changes, t...
The reliable determination of past seawater temperature is fundamental to paleoclimate studies. We t...
The reliable determination of past seawater temperature is fundamental to paleoclimate studies. We t...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
The clumped isotope (Δ47) proxy is a promising geochemical tool to reconstruct past ocean temperatur...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
International audienceAccurate reconstruction of past ocean temperatures is of critical importance t...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
Accurate reconstruction of past ocean temperatures is of critical importance to paleoclimatology. Ca...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
Applying the clumped isotope (Δ47) thermometer to foraminifer microfossils offers the potential to s...
The reconstruction of past ocean temperatures is fundamental to the study of past climate changes, t...
The reliable determination of past seawater temperature is fundamental to paleoclimate studies. We t...
The reliable determination of past seawater temperature is fundamental to paleoclimate studies. We t...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...
Obtaining absolute temperatures of the ocean in deep time is complicated by the lack of constraints ...