Results 171 to 180 of about 42,838 (280)
Planetary sources of bio-essential nutrients on a prebiotic world. [PDF]
Galloway T +3 more
europepmc +1 more source
Multi-technique characterization of iron reduction by an Antarctic <i>Shewanella</i>: an analog system for putative Martian biosignature identification. [PDF]
Shaffer JMC +9 more
europepmc +1 more source
Clay‐based mortar reinforced with coconut fibers showed improved flexural strength and promising mechanical performance, despite shrinkage‐induced cracks. The study highlights the potential of using waste and natural fibers in eco‐efficient mortars, emphasizing the importance of curing and moisture control.
Gabriela Machado Guimarães Ferreira +1 more
wiley +1 more source
Dissecting the puzzle of tectonic lid regimes in terrestrial planets. [PDF]
Lyu T +6 more
europepmc +1 more source
New Zealand's Second Meteorite: Makarewa (find, L4, S5, W2)
One of the most remarkable discoveries of a meteorite in New Zealand was that of Makarewa. Discovered in 1879, Makarewa is a ‘find’ that was uncovered a metre below the surface of a clay bank during excavation works for a train line in the southern South Island.
Mia R. E. Boothroyd +3 more
wiley +1 more source
Widespread terrestrial ecosystem disruption at the onset of the Paleocene-Eocene Thermal Maximum. [PDF]
Nelissen M +7 more
europepmc +1 more source
Evolution of Carbonate Mineralogy Through the CM2-CM1 Series [PDF]
Lee, M.R., Lindgren, P., Sofe, M.R.
core
The deposition of the sandstone sedimentary succession of the Beacon Supergroup lasted more than 200 Myr (Devonian to Early Jurassic) in Victoria Land and nearby territories in the so‐called Transantarctic Basin, recording crucial events in the history of the Earth.
Luca Zurli +7 more
wiley +1 more source
Glacier‐Atmosphere Interactions and Feedbacks in High‐Mountain Regions ‐ A Review
Abstract Mountain glaciers are among the natural systems most vulnerable to climate change. However, their interactions with the atmosphere are complex and not fully understood. These interactions can trigger rapid adjustments and climate feedbacks that either amplify or attenuate atmospheric signals, influencing both glacier response and large‐scale ...
T. Sauter +17 more
wiley +1 more source

