Alessandro Zanazzi

ORCID: 0000-0003-2799-6031
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Pleistocene-Era Hominins and Archaeology
  • Evolution and Paleontology Studies
  • Isotope Analysis in Ecology
  • Archaeology and ancient environmental studies
  • Forensic Anthropology and Bioarchaeology Studies
  • Coastal wetland ecosystem dynamics
  • Peatlands and Wetlands Ecology
  • Marine and environmental studies
  • Groundwater and Isotope Geochemistry
  • Geological and Geochemical Analysis
  • Hydrology and Watershed Management Studies
  • Earthquake and Disaster Impact Studies
  • Animal Ecology and Behavior Studies
  • Archaeological and Geological Studies
  • Ecology and Conservation Studies
  • Bat Biology and Ecology Studies
  • Heavy metals in environment
  • Bryophyte Studies and Records
  • Water Quality Monitoring Technologies
  • Lichen and fungal ecology
  • Groundwater flow and contamination studies
  • Water Quality and Pollution Assessment
  • Morphological variations and asymmetry
  • Image Processing and 3D Reconstruction

Utah Valley University
2014-2024

University of South Carolina
2007

Iowa State University
2005

Utah Lake is one of the largest freshwater bodies in West and a valuable resource for agricultural recreational activities region. However, it has suffered elevated trace metal nutrient levels since pioneer settlement 1847. The objectives this project were as follows: (1) investigate temporal spatial variations concentrations its tributaries; (2) model across lake using GIS analysis techniques. We collected floc layer sediment samples quarterly well monthly water analyses at designated...

10.3390/w16030502 article EN Water 2024-02-04

10.1016/j.palaeo.2007.08.007 article EN Palaeogeography Palaeoclimatology Palaeoecology 2007-09-18

To investigate the hydrology of Utah Lake, we analyzed hydrogen (δ2H) and oxygen (δ18O) stable isotope composition water samples collected from various components its system. The average δ2H δ18O values inlets are similar to groundwater, which in turn has a that is winter precipitation. This suggests snowmelt-fed groundwater main source Valley river waters. In addition, plot close local meteoric line, suggesting no significant evaporation occurring these rivers. contrast, lake outlet have...

10.3390/hydrology7040088 article EN cc-by Hydrology 2020-11-16

To investigate the paleoclimate and paleoenvironment of central Italy during Middle Pleistocene, we analyzed carbon oxygen stable isotope composition carbonate component sequential enamel samples from twenty-four rhinoceros (Stephanorhinus spp.) teeth. The come two key archeological paleontological sites located in Molise region: Isernia La Pineta (ILP; ∼600 ka) Guado San Nicola (GSN; ∼400 ka). Carbon ratios both ILP GSN indicate feeding a pure C3 ecosystem that consisted predominantly...

10.1016/j.quaint.2022.01.011 article EN cc-by-nc-nd Quaternary International 2022-02-23

10.1130/abs/2024am-400580 article EN Abstracts with programs - Geological Society of America 2024-01-01
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