Wolfgang Müller
Goethe University Frankfurt
GeomorphologyGeologyGeochemistryCalciteTrace element
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Publications 116
#1Nina Kowalik (PAN: Polish Academy of Sciences)H-Index: 1
#2Robert Anczkiewicz (PAN: Polish Academy of Sciences)H-Index: 20
Last. Mihály Gasparik (Hungarian Natural History Museum)H-Index: 6
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Mobility of people and goods during the Upper Paleolithic has proven difficult to reconstruct given the relative rareness of remains. Nevertheless, archaeological contexts like the Late Pleistocene horizon of Borsuka Cave (Southern Poland) represent a unique opportunity to explore patterns of objects' transportation across Central Europe. We investigated the origin of four ornaments made of European elk (Alces alces L.) incisors recovered at Borsuka Cave - the oldest known burial site in Poland,...
#1Q. Li (RHUL: Royal Holloway, University of London)
#1Qin Li (RHUL: Royal Holloway, University of London)H-Index: 9
Last. Wolfgang Müller (Goethe University Frankfurt)H-Index: 30
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Dental enamel represents an important mineralized archive of an individual’s early life. Previously, isotopic (Ca) or trace element ratios (Sr/Ca, Ba/Ca) have been used to reveal dietary and weanin...
#1Alessia NavaH-Index: 4
Last. Wolfgang MüllerH-Index: 30
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#1Lisa M. Baldini (Durham University)H-Index: 13
#2James U. L. Baldini (Durham University)H-Index: 21
Last. David A. Richards (UoB: University of Bristol)H-Index: 29
view all 13 authors...
Abstract Several stalagmite records have yielded important but discontinuous insights into northern Iberian climate since the Last Glacial. Here we present the first continuous Iberian stalagmite-based reconstruction of climate since the Bolling-Allerod interstadial, from a single stalagmite sample (GAR-01 from La Garma Cave, Cantabria). The ∼13.5 ka GAR-01 record provides the opportunity for replication, continuation, and aggregation of previously published records from northern Spain. The GAR-...
#1Adam Levi (HUJI: Hebrew University of Jerusalem)
#2Wolfgang Müller (Goethe University Frankfurt)H-Index: 30
Last. Jonathan Erez (HUJI: Hebrew University of Jerusalem)H-Index: 41
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Two species of Amphistegina were cultured under four variable DIC concentrations (2340-2570 M). The variability of trace element within the foraminiferal shells was measured in the knob area of three individuals for each DIC treatment using LA-ICPMS. In individuals that showed significant growth (identified via 135Ba-enriched seawater), B, Na and Sr showed an increase with DIC, while K and Mg were slightly lower or unchanged. Sharp transition zones between natural 135Ba and the ~tenfold increas...
#1Wolfgang Müller (Goethe University Frankfurt)H-Index: 30
#2Alessia Nava (Sapienza University of Rome)H-Index: 4
Last. Luca BondioliH-Index: 27
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Abstract Mammalian dental enamel is a key archive for the reconstruction of past environments. Sequentially mineralizing enamel provides continuous, several year-long records, which spatially-resolved sampling can ‘read’ at seasonal or higher time resolution. Yet it remains underexplored how much an initially incorporated compositional signal is overprinted by the two-stage enamel mineralization process, which affects the finally achievable time-resolution. We report results of a systematic inve...
2 CitationsSource
#1David A.D. EvansH-Index: 46
#2Hagar HauzerH-Index: 2
Last. Jonathan ErezH-Index: 41
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1 Citations
#1Rehemat BhatiaH-Index: 1
#2Daniela N SchmidtH-Index: 35
view all 11 authors...
#1Hagar Hauzer (HUJI: Hebrew University of Jerusalem)H-Index: 2
#2David A.D. Evans (St And: University of St Andrews)H-Index: 46
Last. Jonathan Erez (HUJI: Hebrew University of Jerusalem)H-Index: 41
view all 5 authors...
Abstract Reconstructions of past changes in the seawater calcium concentration (Casw) are critical for understanding the long-term changes in ocean chemistry, the carbon cycle and for accurate application of elemental proxies (El/ Ca CaCO 3 ) in foraminifera (e.g., Mg/Ca as proxy of temperature). Here we show that Na/Ca ratios in foraminiferal shells could be used for reconstructing Casw and Mg/Ca in the past oceans. Ca has a short residence time in the ocean (∼1 My), whereas Na in seawater has ...
6 CitationsSource