Results 61 to 70 of about 8,221 (212)
Abstract The northern extent of Greater India is a critical, yet highly debated, parameter for reconstructing the India‐Asia collision. Previous paleomagnetic estimates, including the fill‐the‐gap and fixed great circle approaches, yield widely varying results, spanning from ∼200 to ∼3,000 km. These large discrepancies stem principally from two primary
Xianwei Jiao +3 more
wiley +1 more source
Late Ordovician (Sandbian) palaeogeography of Laurentia, the distribution of ostracod-bearing localities, and the two faunal provinces (map slightly modified after [22]).
Koen Sabbe (144012) +4 more
core +1 more source
Abstract The paleogeographic position of the South China Block (SCB) during the early Paleozoic and its affiliation with Gondwana remain debated. We report new high‐quality paleomagnetic data from sandstone‐dominated Cambrian Stage 3 strata correlated with the Yu'anshan–Hongjingshao succession collected along the southwestern margin of the SCB ...
Dongmeng Zhang +14 more
wiley +1 more source
Extinction intensity during Ordovician and Cenozoic glaciations explained by cooling and palaeogeography [PDF]
A striking feature of the marine fossil record is the variable intensity of extinction during superficially similar climate transitions. Here we combine climate models and species trait simulations to explore the degree to which differing ...
Lunt, Daniel +32 more
core +1 more source
Simulated Ocean Oxygen Under Miocene Boundary Conditions
Abstract The Miocene Climatic Optimum (MCO; 16.9–14.7 Ma) was a warm interval with atmospheric CO2 ${\text{CO}}_{2}$ comparable to end‐of‐21st‐century projections under intermediate emission scenarios. Proxy records indicate the Oxygen Minimum Zone (OMZ) in the Eastern Tropical Pacific (ETP) was small or non‐existent during the MCO, expanding only when
James R. Berg +5 more
wiley +1 more source
The PRISM4 (mid-Piacenzian) palaeoenvironmental reconstruction [PDF]
The mid-Piacenzian is known as a period of relative warmth when compared to the present day. A comprehensive understanding of conditions during the Piacenzian serves as both a conceptual model and a source for boundary conditions and means of ...
Dowsett, Harry +8 more
core +1 more source
The Vallone Inferno rock-shelter is an archeological site located at 770 m a.s.l. in the Madonie massif in Sicily. This massif is modeled into the Triassic and Oligocene sedimentary rocks of the Imerese Basin.
JUAN MANUEL LÓPEZ-GARCÍA +5 more
doaj +1 more source
TERTIARY PALAEOGEOGRAPHY OF JAPAN
In this treatise, six Palaeogeographic maps of Tertiary Japan are given, representing the different stages of the Tertiary Epoch. To facilitate comparison, those of the three stages of Cretaceous have been added. On each map is shown the distribution of Land and Sea when the sea transgression was the greatest.
openaire +2 more sources
THE CARPATHIAN RIVER SYSTEM IN ROMANIA – GENESIS AND EVOLUTION [PDF]
The present Carpathian valley network is the result of a long and complex process synchronous to the evolutionof the Carpathian orographic system during the Cretaceous – Quaternary period. Among other issues, this studyfocuses on the genesis of the great
MIHAI IELENICZ, LAURA TÎRLĂ
doaj
Reconstruction of the palaeogeographical location of Hainan Island is important for understanding the interaction between Indochina and South China. In this study, we integrate topographic relief, gravity anomalies, and magnetic anomalies, along with ...
Mingming Wang +5 more
doaj +1 more source

