Heiko Pingel

ORCID: 0000-0002-0427-045X
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geology and Paleoclimatology Research
  • Geological and Tectonic Studies in Latin America
  • Geological formations and processes
  • Geological and Geophysical Studies Worldwide
  • earthquake and tectonic studies
  • Geochemistry and Geologic Mapping
  • Hydrocarbon exploration and reservoir analysis
  • Evolution and Paleontology Studies
  • Environmental and Cultural Studies in Latin America and Beyond
  • Geological and Geophysical Studies
  • Landslides and related hazards
  • Pleistocene-Era Hominins and Archaeology
  • Methane Hydrates and Related Phenomena
  • High-pressure geophysics and materials
  • Field-Flow Fractionation Techniques
  • Aeolian processes and effects
  • Groundwater and Isotope Geochemistry
  • Island Studies and Pacific Affairs
  • Archaeology and ancient environmental studies
  • Isotope Analysis in Ecology
  • Metallurgical Processes and Thermodynamics
  • Soil erosion and sediment transport
  • Language, Discourse, Communication Strategies
  • Chemical Reactions and Isotopes

University of Potsdam
2015-2025

The northwest Argentine Andes constitute a premier natural laboratory to assess the complex interactions between isolated uplifts, orographic precipitation gradients, and related erosion sedimentation patterns. Here we present new stratigraphic observations age information from intermontane basin sediments elucidate Neogene Quaternary shortening history associated sediment dynamics of broken Salta foreland. This part Andean orogen, which comprises an array basement‐cored range is located at...

10.1029/2010tc002703 article EN Tectonics 2011-03-15

Rainfall in the central Andes associated with South American Monsoon and Low-Level Jet results from orographic effects on atmospheric circulation exerted by Andean Plateau Eastern Cordillera. However, despite its importance for climate, no reliable records exist that allow decoding evolution of thresholds interactions between topography circulation, especially regarding onset humid conditions inherently dry southern Andes. Here, we employ multi-proxy isotope data lipid biomarkers, pedogenic...

10.1038/srep35678 article EN cc-by Scientific Reports 2016-10-21

Abstract The intermontane Quebrada de Humahuaca Basin (Humahuaca Basin) in the Eastern Cordillera of southern Central Andes NW Argentina (23°–24°S) records evolution a formerly contiguous foreland‐basin setting to an depositional environment during late stages Cenozoic Andean mountain building. This basin has been and continues be subject shortening surface uplift, which resulted establishment orographic barrier for easterly sourced moisture‐bearing winds along its eastern margin, followed...

10.1111/bre.12016 article EN Basin Research 2012-12-13

Research Article| August 01, 2014 Pliocene orographic barrier uplift in the southern Central Andes Heiko Pingel; Pingel 1Institut für Erd- und Umweltwissenschaften, Universität Potsdam, 14476 Germany Search for other works by this author on: GSW Google Scholar Ricardo N. Alonso; Alonso 2Departamento de Geología, Universidad Nacional Salta, 4400-Salta, Argentina Andreas Mulch; Mulch 3Institut Geowissenschaften, Goethe Frankfurt, 60438 Frankfurt/Main, Germany4Biodiversität Klima...

10.1130/g35538.1 article EN Geology 2014-07-01

ABSTRACT Sedimentary basins in the distal Cenozoic Andean retroarc yield an important geological archive that provides crucial insights into tectonic and sedimentary processes associated with different stages of mountain building. At 33° S, have operated during Neogene Quaternary periods orogenesis are well documented, whereas information on Paleogene period remains fragmentary partly enigmatic. The sedimentation at this latitude is represented by Divisadero Largo Formation, a 70‐m‐thick...

10.1111/bre.70021 article EN Basin Research 2025-01-01

Abstract The Gofa Province and Chew Bahir Basin in the Broadly Rifted Zone (BRZ) between southern Main Ethiopian Rift (sMER) northern Kenya (nKR) record early volcanism associated faulting East Africa; however, spatiotemporal relationships remain poorly constrained. We applied apatite (U‐Th)/He (AHe) zircon (ZHe) thermochronometry to Neoproterozoic basement rocks from exhumed footwall blocks of extensional Basin, analyzed our result context well‐dated regional volcanic units BRZ unravel...

10.1029/2022tc007651 article EN cc-by Tectonics 2024-01-01

We present stable hydrogen-isotope analyses of volcanic glass ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline" overflow="scroll"><mml:mi mathvariant="normal">δ</mml:mi></mml:math> Dg) and radiometric ages (U–Pb zircon, U–Th calcite, AMS 14 C) from deformed sedimentary deposits in the vicinity intermontane Pocitos Basin central Puna Andean Plateau at about 24.5°S. Our results demonstrate 2-km surface uplift since middle to late Miocene protracted shortening that...

10.1073/pnas.2303964120 article EN cc-by-nc-nd Proceedings of the National Academy of Sciences 2023-10-09

Abstract The Andean Plateau of NW Argentina is a prominent example high‐elevation orogenic plateau characterized by internal drainage, arid to hyper‐arid climatic conditions and compressional basin‐and‐range morphology comprising thick sedimentary basins. However, the development as geomorphic entity not well understood. Enhanced orographic rainout along eastern, windward flank causes reduced fluvial run‐off thus subdued surface‐process rates in hinterland. Despite this, many Puna basins...

10.1111/bre.12346 article EN Basin Research 2019-02-11

Abstract The structural and topographic evolution of orogenic plateaus is an important research topic because its impact on atmospheric circulation patterns, the amount distribution rainfall, resulting changes in surface processes. Puna region north‐western Argentina (between 13°S 27°S) part Andean Plateau, which world's second largest plateau. In order to investigate deformational events responsible for initial growth this plateau, we carried out stratigraphic investigations within...

10.1111/bre.12510 article EN Basin Research 2020-09-20

Abstract The Andean Plateau of north‐western Argentina (Puna) at a mean elevation ca. 4.2 km constitutes the southern continuation Altiplano; it is compressional basin‐and‐range province comprising fault‐bounded, high‐elevation mountain ranges and largely internally drained basins with often thick sedimentary volcaniclastic fill. Growing sedimentological structural evidence supports notion that Argentine Andes between 22° 26°S developed from an initial extensive broken‐foreland system...

10.1029/2022tc007487 article EN cc-by Tectonics 2023-01-21

Research Article| February 26, 2019 Pliocene–Pleistocene orographic control on denudation in northwest Argentina Heiko Pingel; Pingel 1Institut für Geowissenschaften, Universität Potsdam, Karl-Liebknecht-Strasse 24-25, 14476 Germany Search for other works by this author on: GSW Google Scholar Taylor Schildgen; Schildgen Germany2Helmholtz Centre Potsdam–GFZ German Geosciences, Telegrafenberg, 14473 Manfred R. Strecker; Strecker Hella Wittmann 2Helmholtz Author and Article Information...

10.1130/g45800.1 article EN Geology 2019-02-26

Abstract Foreland basins are sensitive recorders of spatiotemporal variations in tectonic and climatic forcing associated with an approaching orogenic front. Thus, analysis foreland deposits their deformation patterns provenance signals allows assessment sedimentary processes during orogeny, providing clues to past environmental conditions. The Calchaquí region the southern part northwest Argentinian Eastern Cordillera (ca. 25–26°S lat) structurally evolved from a contiguous Paleogene Andes...

10.1111/bre.12589 article EN Basin Research 2021-07-28

Informal verbal interaction is the core matrix for human social life. A mechanism coordinating this basic mode of a system turn-taking that regulates who to speak and when. Yet relatively little known about how ...

10.1073/pnas.2406845121 article EN cc-by-nc-nd Proceedings of the National Academy of Sciences 2024-05-20

Abstract The thick‐skinned fold‐and‐thrust belt on the eastern flank of Andean Plateau in northwestern Argentina (NWA) is a zone active contractional deformation characterized by fault‐bounded mountain ranges with no systematic spatiotemporal pattern tectonic activity. In contrast, thin‐skinned Subandean northern and southern Bolivia primarily in‐sequence (i.e., west to east) fault progression, narrow Quaternary focused at front orogenic wedge. To better understand how recent accommodated...

10.1029/2020tc006394 article EN cc-by-nc Tectonics 2020-12-07

Abstract Compared to the thin‐skinned Subandean foreland fold‐and‐thrust belt of northern Argentina and Bolivia, tectonically active morphotectonic province Santa Bárbara System in Andean broken northwestern is characterized by a temporally spatially disparate deformation style. Although there no well‐defined orogenic front associated with uplift these basement‐cored, reverse‐fault bounded mountain ranges, has been an overall eastward trend compressional since Miocene. While reactivation...

10.1029/2023tc008195 article EN cc-by-nc-nd Tectonics 2024-06-01
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