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Paleosols, bones, phytoliths, and δ13C signatures of humus and teeth in the alluvial sequence of Axamilpa, Puebla : Inferences for landscape evolution and megafauna paleoecology during MIS 3–2 in Southern Mexico
  • Paleosols, bones, phytoliths, and δ13C signatures of humus and teeth in the alluvial sequence of Axamilpa, Puebla : Inferences for landscape evolution and megafauna paleoecology during MIS 3–2 in Southern Mexico
  • Landscapes and soils through time
  • (stable carbon isotopes and phytoliths) and mammalian fossil remains incorporated in an alluvial paleosol-sedimentary sequence. The AA. interpret the Late Pleistocene landscape of this area as a heterogeneous forest–grassland landscape with the forest
Late Pleistocene–Holocene environmental changes in ultra-continental subarid permafrost-affected landscapes of the Terekhol' Basin, South Siberia
  • Late Pleistocene–Holocene environmental changes in ultra-continental subarid permafrost-affected landscapes of the Terekhol' Basin, South Siberia
  • Landscapes and soils through time
  • This study is an attempt to use closely related inter-complementary paleo-archives of a local landscape to access understanding of Late Pleistocene–Holocene environmental changes in the region. The study site is a small intermountain basin
The evidence of lateral podzolization in sandy soils of Northern Poland
  • Landscapes and soils through time
  • Evidence of slope-scale element translocation (lateral podzolization) has been documented in sandy areas of Northern Poland. Landscape position and features of the studied soils suggest inter-pedon translocation of organic matter, iron and aluminum
Palustrine carbonates and pedogenic calcretes in the Çal basin of SW Anatolia : Implications for the Plio-Pleistocene regional climatic pattern in the eastern Mediterranean
  • Landscapes and soils through time
  • δ18 O-δ13 C may indicate subhumid conditions or significant diagenetic alteration. The δ13 C values of these carbonates, organic δ13 C data from calcretes and floral remains indicate that the landscapes were dominated by C3 forest plants.
Buried black soils on the slopes of Mt. Kilimanjaro as a regional carbon storage hotspot
  • Landscapes and soils through time
Red Mediterranean Soils in Jordan : New insights in their origin, genesis, and role as environmental archives
  • Landscapes and soils through time
Palaeoecological reconstruction of wetlands and Eneolithic land use in Ljubljansko barje (Slovenia) based on biomorphic and pollen analysis
  • Landscapes and soils through time
Thin-section analysis of lithified paleosols from Dagshai Formation of the Himalayan Foreland : Identification of paleopedogenic features and diagenetic overprinting and implications for paleoenvironmental reconstruction
  • Landscapes and soils through time
The development of deep soil processes in ancient kurgans of the North Caucasus
  • Landscapes and soils through time
Quaternary paleosols and sediments on the Balearic Islands as indicators of climate changes
  • Landscapes and soils through time
The effect of pedological conditions on the sources and sinks of silicon in the Vertic Planosols in south-western Ethiopia
  • Landscapes and soils through time
Stable isotopic composition of carbonate pedofeatures in soils along a transect in the southern part of European Russia
  • Landscapes and soils through time
Lateral and depth variation of loess organic matter overprint related to rhizoliths — Revealed by lipid molecular proxies and X-ray tomography
  • Landscapes and soils through time