By the late Eocene and early Oligocene, Canarieae had diversified in Southeast Asia, coinciding with rise of the roughly 20,000 landmasses of the IAA and the formation of modern tropical cyclone pathways and fast westward-moving equatorial surface currents (Figs. 2 and 3) that created opportunities for marine LDD [ 10, 47, 49].
The spores are actinomorphic and trilete with polar surface triangles, and the equatorial surface is semicircular or super-semicircular.
For the objects with atmospheres (Titan and all of the planets except Mercury) we estimate the total neutral gas mass, M, as where R is the object radius, p is the atmospheric pressure at the surface, and g is the equatorial surface gravity.
Distribution of epithermal neutron flux and hydrogen content from equatorial surface of the Moon, obtained by neutron spectrometers LEND and LPNS is studied.
Additionally, the equatorial surface is semicircular or super-semicircular, and the surface ornamentation is psilate [ 11].
Our study illustrates the importance of considering long distance dispersal as a viable explanation for clades with pantropical distributions diversifying subsequent to the Oligocene, and it highlights the formation of the Indo-Australian Archipelago and associated fast-moving equatorial surface currents, suggesting an under-appreciated evolutionary link among tropical centers of endemism.
Equatorial surface waters were then able to circumnavigate the world and became even warmer.
The field would have an equatorial surface field strength of approximately 719 nT (Kivelson et al. 2002).
Earlier experiments from this laboratory used a conventional divided chamber, which occluded the equatorial surface, to demonstrate that anterior applications of ACh transiently decreased the ISC due to an intracellular Ca2+ release and inhibition of anteriorly located K+ channels.
On the long field lines examined in this work (at the L ~ 5 10 magnetic shells) the oscillation amplitude is maximum near the equatorial surface decreasing rapidly away from it.
