Sentence examples for distribution of continents from inspiring English sources

For palaeontologists, there could be a tendency to view life in terms of vicariance, particularly driven by the ancient distribution of continents and plate-tectonic shifts.

The Triassic Period marked the beginning of major changes that were to take place throughout the Mesozoic Era, particularly in the distribution of continents, the evolution of life, and the geographic distribution of living things.

These factors include variations in solar radiation due to latitude, distribution of continents and oceans, atmospheric pressure and wind systems, ocean currents, major terrain features, proximity to water bodies, and local features including topography.

Global plate motion models indicate that the distribution of continents has evolved from a spherical harmonic degree-1 heterogeneity before the breakup of supercontinent Pangea to its present-day degree-2 structure (Seton et al. 2012).

This layer captures the non-uniform distribution of the continents and oceans.

The authors assume that the phenomenon can be related to the asymmetric distribution of the continents and oceans between the hemispheres and/or with the asymmetry of the geographic field to the geomagnetic field.

Moreover, we demonstrate that the Congo drainage system plays a central role in the distribution of the continent's freshwater fauna during the late Cenozoic.

Nevertheless, the geographical distribution of the mentioned continents is reflected in our dataset, excluding only some minor actors.

The surface shell (taken from Manoj et al. [2006]) accounts for the distribution of oceans and continents as well as sediment thicknesses.

We present an inversion scheme to recover the (1-D) depth profile of mantle conductivity from satellite magnetic data, which takes into account 3-D effects arising from the distribution of oceans and continents.

Most recently, Kuvshinov and Olsen (2006) derived a global model of mantle conductivity from five years of CHAMP, Ørsted and SAC-C magnetic data and demonstrated the necessity of taking into account the contributions of a laterally heterogeneous surface shell representing the distribution of oceans and continents.