Science & Technology
Humans spend a lot of time and energy choosing their partner. A new study by researchers from Stockholm University and Manchester University NHS Foundation Trust (MFT) shows that choosing your partner continues even after sex — human eggs can "choose" sperm.
"Human eggs release chemicals called chemoattractants that attract sperm to unfertilized eggs. We wanted to know if eggs use these chemical signals to pick which sperm they attract," said John Fitzpatrick, an Associate Professor at Stockholm University.
The researchers examined how sperm respond to follicular fluid, which surrounds eggs and contains sperm chemoattractants. The researchers wanted to find out if follicular fluids from different females attracted sperm from some males more than others.
During their 3,000-year dominance over Mesoamerica, the Mayans built elaborate architectural structures and developed a sophisticated, technologically progressive society. But immediately after reaching the peak of its powers over the entire Yucatan Peninsula, the Mayan Empire collapsed, falling apart in just 150 years. The reasons for its sudden demise remain a mystery, but in a new Science study, scientists find clues buried deep in the mud of Lake Chichancanab.
Deforestation, overpopulation, and extreme drought have all been proposed as the reason for the empire's collapse. The most probable of those, argue the University of Cambridge and University of Florida scientists in the new study, is drought. The evidence they gathered in the muddy sediments underlying Lake Chichancanab, which was once a part of the empire, underscore the devastating power of a drought on a population.

Deep beneath the Marquesas Islands in the South Pacific is a giant structure near Earth’s core
Analysing data from hundreds of major earthquakes, Doyeon Kim at the University of Maryland and his colleagues have found a new structure beneath the volcanic Marquesas Islands in the South Pacific Ocean. The structure, known as an ultra-low velocity (ULV) zone, is about 1000 kilometres in diameter and 25 kilometres thick, says Kim.
These structures are called ULV zones because seismic waves pass through them at slower velocities, but what they are made of is still a mystery. They might be chemically distinct from Earth's iron-nickel alloy core and silicate rock mantle, or have different thermal properties.
The researchers discovered the structure while analysing 7000 records of seismic activity from earthquakes that occurred around the Pacific Ocean basin between 1990 and 2018. The earthquakes all had a magnitude of 6.5 or greater, and were all deeper than 200 kilometres below Earth's surface.
The giant extinct invertebrate Arthropleura resembled some modern millipedes, but could grow to be more than one-and-a-half feet wide, and may sometimes have been more than six feet long. Reconstruction of the giant millipede Arthropleura from the Pennsylvanian and earliest Permian of North America and Europe.
During the Pennsylvanian and earliest Permian periods (about 320 to 290 million years before present), much of present-day North America and Europe was located close to the equator and was covered by vast, richly vegetated swamps.
The cause?
Most likely the cracks are from wide variations in temperatures, with sunlight heating up the rocks during the day, and then cooling off quickly at night. This process happens quickly and frequently, as Bennu makes one full rotation on its axis every 4.3 hours.
"This is the first time evidence for this process, called thermal fracturing, has been definitively observed on an object without an atmosphere," said Jamie Molaro of the Planetary Science Institute in Tucson, Arizona. Molaro is the lead author of a paper published today in Nature Communications. "It is one piece of a puzzle that tells us what the surface used to be like, and what it will be like millions of years from now."
Comment: The cause of the cracking is stated to 'likely' be due to thermal fracturing, and it may be, but one should also bear in mind the other forces at work on space bodies:
- Comet 67P surprises scientists with 'bright outbursts', collapsing cliffs and rolling boulders during Rosetta mission
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- Behind the Headlines: Earth changes in an electric universe: Is climate change really man-made?
- Adapt 2030 Ice Age Report: Interview with Laura Knight-Jadczyk and Pierre Lescaudron
They took atoms of a soft metal called rubidium, and cooled them to temperatures around 100 nanoKelvin - one ten-millionth of a Kelvin above absolute zero.
This resulted in a super cold cloud called a Bose-Einstein condensate, the exotic 'fifth' state of matter, and one that could help us understand the weird quantum properties of ultra-cold atoms. But the research did not stop there.
Using the Jet Propulsion Laboratory's Cold Atom Laboratory, scientists went on to produce Bose-Einstein condensates less than a nanoKelvin above absolute zero - exploiting the microgravity conditions aboard the space station to learn more about this state than we could on Earth.

The colors in this newly discovered phase of liquid crystal shift as researchers apply a small electric field.
The team describes the discovery of what scientists call a "ferroelectric nematic" phase of liquid crystal in a study published today in the Proceedings of the National Academy of Sciences. The discovery "opens a door to a new universe of materials," said co-author Matt Glaser, a professor in the Department of Physics.
Nematic liquid crystals have been a hot topic in materials research since the 1970s. These materials exhibit a curious mix of fluid- and solid-like behaviors, which allow them to control light. Engineers have used them extensively to make the liquid crystal displays (LCDs) in many laptops, TVs and cellphones.
Think of nematic liquid crystals like dropping a handful of pins on a table. The pins in this case are rod-shaped molecules that are "polar" — with heads (the blunt ends) that carry a positive charge and tails (the pointy ends) that are negatively charged. In a traditional nematic liquid crystal, half of the pins point left and the other half point right, with the direction chosen at random.
A ferroelectric nematic liquid crystal phase, however, is much more disciplined. In such a liquid crystal, patches or "domains" form in the sample in which the molecules all point in the same direction, either right or left. In physics parlance, these materials have polar ordering.
Noel Clark, a professor of physics and director of the SMRC, said that his team's discovery of one such liquid crystal could open up a wealth of technological innovations — from new types of display screens to reimagined computer memory.
"There are 40,000 research papers on nematics, and in almost any one of them you see interesting new possibilities if the nematic had been ferroelectric," Clark said.

In experiments at the National Ignition Facility, a SLAC-led team found new details about how supernovas boost charged particles to nearly the speed of light.
Now, scientists have devised a new way to study the inner workings of astrophysical shock waves by creating a scaled-down version of the shock in the lab. They found that astrophysical shocks develop turbulence at very small scales - scales that can't be seen by astronomical observations - that helps kick electrons toward the shock wave before they're boosted up to their final, incredible speeds.

Three water-filled maars in the Eifel, Germany (Gemündener Maar, Weinfelder Maar, Schalkenmehrener Maar). Created by volcanic activity, maars are also found in other parts of Europe and on other continents, but Eifel-Maars are the classic example worldwide.
The Eifel region lies roughly between the cities of Aachen, Trier, and Koblenz, in west-central Germany. It is home to many ancient volcanic features, including the circular lakes known as 'maars'.
These are the remnants of violent volcanic eruptions, such as the one which created Laacher See, the largest lake in the area. The explosion that created this is thought to have occurred around 13,000 years ago, with a similar explosive power to the cataclysmic Mount Pinatubo eruption in 1991.
The mantle plume that likely fed this ancient activity is thought to still be present, extending up to 400km down into the Earth. However, whether or not it is still active is unknown: "Most scientists had assumed that volcanic activity in the Eifel was a thing of the past," said Prof. Corné Kreemer, lead author of the new study. "But connecting the dots, it seems clear that something is brewing underneath the heart of northwest Europe."

Artwork of Saturn, Titan, and the Cassini spacecraft.
Now, decades of measurements and calculations have revealed that Titan's orbit around Saturn is expanding — meaning, the moon is getting farther and farther away from the planet — at a rate about 100 times faster than expected. The research suggests that Titan was born much closer to Saturn and migrated out to its current distance of 1.2 million kilometers (about 746,000 miles) over 4.5 billion years.
The findings are described in a paper that appears in the journal Nature Astronomy on June 8.
"Most prior work had predicted that moons like Titan or Jupiter's moon Callisto were formed at an orbital distance similar to where we see them now," says Caltech's Jim Fuller, assistant professor of theoretical astrophysics and co-author on the new paper. "This implies that the Saturnian moon system, and potentially its rings, have formed and evolved more dynamically than previously believed."











Comment: See also: SOTT Exclusive: A 'Blue Hole,' a cosmic connection and the demise of the Maya