The remote sensing imagery below, metaphorically akin to an ultrasound, show La Niña in the womb. The climate phenomenon's due date is fast arriving.

Matt Wright and Charlie Demers make waves in St. John’s, Newfoundland when they discuss if the Atlantic Ocean is superior to the Pacific Ocean. Then, Bree Parsons and Nikki Payne bring a wealth of wit when they decide if growing up poor makes you a stronger person.

Title: Scientists Pinpoint Source of Mercury in Pacific Ocean Fish
Category: Health News
Created: 8/26/2013 9:35:00 AM
Last Editorial Review: 8/26/2013 12:00:00 AM

Archives, Room Use Only - TK5613.C36 1900

Archives, Room Use Only - HE2763.U55 1867

Archives, Room Use Only - HE2763.P33 1868

The bottom of the Pacific Ocean is actually cooling down. How is this possible? The answer is proof that Earth's systems operate on long timescales.

I've been covering the Great Pacific Garbage Patch for the past year or so and just wrote about it here on MNN last week.

Scientists from the Scripps Institution of Oceanography traveled out to a spot of sea 1,000 miles from shore and were sad to find plastic everywhere.

A huge sea of plastic trash is swirling in the North Pacific — part of an even broader plastic plague that's growing in oceans worldwide.

More than 3,000 World War II wrecks lie in the Pacific Ocean of which around 300 are oil tankers. There are fears of environmental devastation as they begin to rust and leak oil.

Assemblages of upper lower through upper Miocene Discoaster spp. have been quantified from Integrated Ocean Drilling Program (IODP) Site U1338 in the eastern equatorial Pacific Ocean. These assemblages can be grouped into five broad morphological categories: six-rayed with bifurcated ray tips, six-rayed with large central areas, six-rayed with pointed ray tips, five-rayed with bifurcated ray tips and five-rayed with pointed ray tips. Discoaster deflandrei dominates the assemblages prior to 15.8 Ma. The decline in abundance of D. deflandrei close to the early–middle Miocene boundary occurs together with the evolution of the D. variabilis group, including D. signus and D. exilis. Six-rayed discoasters having large central areas become a prominent member of the assemblages for a 400 ka interval in the late middle Miocene. Five- and six-rayed forms having pointed tips become prominent in the early late Miocene and show a strong antiphasing relationship with the D. variabilis group. Discoaster bellus completely dominates the Discoaster assemblages for a 400 ka interval in the middle late Miocene. Abundances of all discoasters, or discoasters at the species level, show only (surprisingly) weak correlations to carbonate contents or oxygen and carbon isotopes of bulk sediment when calculated over the entire sample interval.