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Augusto Mangini

Researcher at Heidelberg University

Publications -  194
Citations -  13109

Augusto Mangini is an academic researcher from Heidelberg University. The author has contributed to research in topics: Stalagmite & Speleothem. The author has an hindex of 58, co-authored 194 publications receiving 12183 citations.

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Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman.

TL;DR: A high-resolution oxygen-isotope record from a thorium-uranium–dated stalagmite from southern Oman reflects variations in the amount of monsoon precipitation, indicating that early Holocene monsoon intensity is largely controlled by glacial boundary conditions.
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Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra)

TL;DR: In this article, high-resolution oxygen isotope (δ18O) profiles of Holocene stalagmites from four caves in Northern and Southern Oman and Yemen (Socotra) provide detailed information on fluctuations in precipitation along a latitudinal transect from 12°N to 23°N.
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Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago

TL;DR: A high-resolution record of oxygen isotope variations, for the period from 9.6 to 6.1 kyr before present, in a Th–U-dated stalagmite from Oman suggests that one of the primary controls on centennial- to decadal-scale changes in tropical rainfall and monsoon intensity during this time are variations in solar radiation.
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Reconstruction of temperature in the Central Alps during the past 2000 yr from a δ18O stalagmite record

TL;DR: In this article, the precisely dated isotopic composition of a stalagmite from Spannagel Cave in the Central Alps is translated into a highly resolved record of temperature at high elevation during the past 2000 yr.
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Changing moisture sources over the last 330,000 years in Northern Oman from fluid-inclusion evidence in speleothems

TL;DR: In this paper, a record of continental pluvial periods over the last 330,000 yr was provided by speleothems from Hoti Cave in northern Oman, where the authors measured the δD values of water extracted from speleothem fluid inclusions (δDFI) and calculated δ18O values of calcite calcite.