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Gerald H. Haug

Researcher at Max Planck Society

Publications -  198
Citations -  20379

Gerald H. Haug is an academic researcher from Max Planck Society. The author has contributed to research in topics: Glacial period & Holocene. The author has an hindex of 60, co-authored 184 publications receiving 17516 citations. Previous affiliations of Gerald H. Haug include ETH Zurich & Woods Hole Oceanographic Institution.

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Mg/Ca-temperature calibration for the benthic foraminifera Melonis barleeanum and Melonis pompilioides

TL;DR: Foraminifera of the genus Melonis appeared to be promising candidates for temperature reconstruction due to their wide geographical and bathymetric distribution, and their infaunal habitat, which was suggested to reduce secondary effects from carbonate ion saturation (Δ[CO3 2−]). as discussed by the authors made substantial advances to previous calibration efforts and presented new multi-lab Mg/Ca data for Melonis barleeanum and Melonis pompilioides from more than one hundred core top samples spanning in situ bottom temperatures from −1 to 16 °C, coupled with morph
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Size-specific opal-bound nitrogen isotope measurements in North Pacific sediments

TL;DR: In this article, the nitrogen isotope composition of diatom opal (δ 15 N db ) was measured by separating the opal from subarctic Pacific and Bering Sea sediments from the Holocene back to the last glacial.
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Comment on “On linking climate to Chinese dynastic change: Spatial and temporal variations of monsoonal rain”

TL;DR: Zhang et al. as mentioned in this paper pointed out that their approach lacks logical rigor and their major argument is broadly consistent with, rather than contradictory to, their original conclusions, and pointed out the fact that climate-culture relationships similar to those observed in China have been observed for other cultures around the world.