Results 171 to 180 of about 10,064 (318)
Low‐relief dry channels appear out of place across a glaciated karst landscape in northern Ohio. Channels are only a few metres deep cut into limestone and draped with a veneer of till. Several hypotheses are proposed for explaining the channels. Low‐relief dry channels are observed across the Bellevue‐Castalia Karst Plain of north‐central Ohio, USA ...
Timothy G. Fisher+6 more
wiley +1 more source
Taphonomic Trajectory of Diagenesis: How Site Formation Should Inform Biological Sampling Strategies for Isotopic Studies of Ancestors. [PDF]
Beasley MM.
europepmc +1 more source
Palaeoecological studies reporting long‐term development histories of subarctic fens—explicitly, orohemiarctic peatlands—are scarce, and overall, permafrost‐free peatlands located in the immediate vicinity of permafrost zones have received little attention in Fennoscandia. Here, we use a multiproxy approach to study the millennial‐scale dynamics of two
Sanna R. Piilo+6 more
wiley +1 more source
Identification and cleaning of an onion-based residue in a historical layer of Giacomo Balla's Ritratto d'uomo / Eugenio Riva. [PDF]
Macchia A+3 more
europepmc +1 more source
Persistence and dynamic of forest snails in the Western Carpathians over the last 40 thousand years
The glacial/interglacial cycles have shaped the landscape of temperate Europe for the past 2.5 million years, with open landscapes prevailing during the glacial and forested landscapes during the interglacial periods. However, the survival and recolonization strategies of temperate forest species during glacial phases remain poorly understood and hotly
Lucie Juřičková+5 more
wiley +1 more source
Microfacies analysis and diagenetic history of Lower to Middle Eocene carbonates at Umm Russies area in the northeastern desert of Egypt. [PDF]
Abd-Elhameed M+4 more
europepmc +1 more source
ABSTRACT: High Resolution Sequence Stratigraphy on a Geologic Workstation
William C. Ross
openalex +1 more source
Sequence stratigraphy of the Nukumaruan Stratotype (Pliocene‐Pleistocene, c. 2.08–1.63 Ma), Wanganui Basin, New Zealand [PDF]
Steve Abbott+3 more
openalex +1 more source