«Excavating plant fossils preserved in
rocks deposited during the last days of the dinosaurs, we found some preserved with abundant fossilized charcoal and others without it.
By looking at the chemistry of
rocks deposited during that time period, specifically coupled carbon and sulfur isotope data, a research team led by University of California, Riverside biogeochemists reports that oxygen - free and hydrogen sulfide - rich waters extended across roughly five percent of the global ocean during this major climatic perturbation — far more than the modern ocean's 0.1 percent but much less than previous estimates for this event.
Not exact matches
The fossil was recovered from sedimentary
rock strata that were
deposited in an ancient lake roughly 55 million years ago,
during the early part of the Eocene epoch.
Calcite precipitates out of pressurized fluids that travel through
rock near faults
during some earthquakes and gets
deposited in layers, like rings of a tree.
«Dinosaur remains from the Arabian Peninsula and the area east of the Mediterranean Sea are exceedingly rare because sedimentary
rocks deposited in streams and rivers
during the Age of Dinosaurs are rare, particularly in Saudi Arabia itself» says Dr Tom Rich from Museum Victoria in Australia.
The latter events left behind distinctive
rock - sequences typically consisting of tillites (ancient boulder - clay, now solid
rock) representing ice -
deposited debris, overlain with a depositional break by cap - carbonates (chemical sediments of marine origin
deposited during interglacials following global sea - level rises).
Bright features such as these are caused by the presence of freshly crushed
rock material that was excavated and
deposited during the highly energetic collision of a meteoroid with Mercury to form an impact crater.
They found that the diatom - rich sediments,
deposited during the warm intervals, were predominantly composed of material from one terrane - the Jurassic to Cretaceous volcanic
rocks and associated sedimentary
rocks of the Ferrar Large Igneous Province (FLIP).
The latter events left behind distinctive
rock - sequences typically consisting of tillites (ancient boulder - clay, now solid
rock) representing ice -
deposited debris, overlain with a depositional break by cap - carbonates, chemical sediments of marine origin
deposited during interglacials following global sea - level rises.