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2014 Napa earthquake continued to creep

On August 24, 2014, just south of Napa, California, a fault in the Earth suddenly slipped, violently shifting and splitting huge blocks of solid rock, 6 miles below the surface.

The underground upheaval generated severe shaking at the surface, lasting 10 to 20 seconds. When the shaking subsided, the magnitude 6.0 earthquake—the largest in the San Francisco Bay Area since 1989—left in its wake crumpled building facades, ruptured water mains, and fractured roadways.

But the earthquake wasn’t quite done. In a new report, scientists from MIT and elsewhere detail how, even after the earthquake’s main tremors and aftershocks died down, earth beneath the surface was still actively shifting and creeping—albeit much more slowly—for at least four weeks after the main event. This postquake activity, which is known to geologists as “afterslip,” caused certain sections of the main fault to shift by as much as 40 centimeters in the month following the main earthquake.

This seismic creep, the scientists say, may have posed additional infrastructure hazards to the region and changed the seismic picture of surrounding faults, easing stress along some faults while increasing pressure along others.

The scientists, led by Michael Floyd, a research scientist in MIT’s Department of Earth, Atmospheric and Planetary Sciences, found that sections of the main West Napa Fault continued to slip after the primary earthquake, depending on the lithology, or rock type, surrounding the fault. The fault tended to only shift during the main earthquake in places where it ran through solid rock, such as mountains and hills; in places with looser sediments, like mud and sand, the fault continued to slowly creep, for at least four weeks, at a rate of a few centimeters per day.

The world is ‘perilously close’ to irreversible climate change. 5 tipping points keep scientists up at night

Five years ago, the United Nations’ panel on climate change was charged with drafting a series of reports detailing its science, the effects on the planet and how humanity might save itself.

The last of those reports arrived this week, and the news is dire. The world’s scientists say the crisis is upon us, and unless we act now, multiple crucial planetary systems are on the cusp of permanent damage.

“We can’t kick this can down the road any longer,” said Andrea Dutton, a geoscientist at the University of Wisconsin, Madison.

Since the 1880s, the Earth’s temperature has risen more than 2 degrees, according to NASA. That may not sound like a lot, but it’s enough to disrupt natural systems that support all living things—including humans.

In a damning speech Monday, U.N. Secretary-General António Guterres said the world is “perilously close to tipping points that could lead to cascading and irreversible” consequences.

Here are five tipping points scientists say could start to teeter in our children’s lifetime:

Amazon rainforest becomes a savanna

In most immediate peril is the Amazon rainforest.

The 2.5 million square mile rainforest is so vast it creates its own rainfall and is home to 10% of the world’s species.

But rising temperatures and increasing drought are bringing it ever closer to crossing the threshold from lush rainforest to arid savannah.

“The recent evidence has been quite alarming. It really does look like we’re closing in on a place where a relatively modest amount of drying could kill off the rainforest and turn it into something else,” said Daniel Swain, a climate scientist at the University of California, Los Angeles.

In part because of the increased heat and lack of rain, the Amazon is seeing more wildfires. These destroy large areas that grow back not as rainforest but as grasslands with few trees. Illegal logging to grow grass or soybeans to feed cattle exacerbates the problem.

A study published last month found signs of lost habitat in more than 75% of the rainforest since the early 2000s, A 2020 paper estimated as much as 40% of the existing rainforest might not grow back if destroyed.

Coral reefs die

Coral reefs hang in the balance.

Coral are vital to the health of the oceans. Although they cover only 0.2% of the ocean floor, they are home to at least a quarter of all marine species. They provide safety for juvenile fish and are home to the small organisms and fish which provide food for larger fish. Scientists estimate that the reefs account for 25% of fish caught in developing countries.

Coral reefs can survive within only a relatively narrow temperature band. The coral that build them get much of their food from algae living in their tissues. When the seawater is too warm, the coral’s stress response is to expel algae, causing the coral to turn white. The process is called coral bleaching, and if it lasts too long, the coral can starve—turning a thriving ecosystem into a cemetery of dead shells.

A report released last year showed that almost 15% of the planet’s reefs have vanished since 2009, primarily because of climate change.

“They’re being cooked to death,” said Dutton, a MacArthur Genius Award winner, who studies the deep history of the oceans.

“The frequency at which we’re seeing these bleaching events is astounding to those of us who study them,” she said. “It’s going to have a huge domino effect on marine systems and on humans.”

Ice sheets melting

Time is running out for the world’s largest ice sheets.

Both the Antarctic and Greenland ice sheets are melting, and the Antarctic is believed to be the most unstable.

If they melt entirely, it would cause catastrophic sea level rise around the globe. Loss of the Antarctic sheet could result in as high as 11 feet of rise. Loss of the Greenland sheet could be 23 feet, said Timothy Lenton, chair of climate change and Earth system science at the University of Exeter, United Kingdom.

“About 90% of the transportation worldwide goes over the ocean and all port infrastructure is at sea level—you can see what a problem this will cause,” said Peter Schlosser, director of the Global Futures Laboratory at Arizona State University.

Though the rise probably will take much longer, it could happen as quickly as 100 years from now for Antarctica and 300 years for Greenland, a paper by Lenton found.

“I know that might seem a long way off, but you’d be talking about having to move many coastal megacities in the next 100 or 150 years,” he said.

Atlantic circulation stops

The circulation of the Atlantic is at risk.

The official name of this danger is Atlantic Thermohaline Circulation Collapse. If it were to happen, it could bring about an ice age in Europe and sea level rise in cities like Boston and New York.

What’s known as the Atlantic Meridional Overturning Circulation (AMOC) keeps warmer water from the tropics flowing north along the coast of northern Europe to the Arctic, where it cools and sinks to the bottom of the ocean. That cooler water is then pulled back southward along the coast of North America as part of a circular pattern.

This cycle keeps northern Europe several degrees warmer than it would otherwise be and brings colder water to the coast of North America.

There is some indication the system has experienced a gradual weakening over the past few decades, and it may be critically unstable.

Lenton’s research suggests that if global temperatures continue to rise, the AMOC could collapse in 50 to 250 years.

The 2019 IPCC report suggested the AMOC will “very likely” weaken this century but has a less than 10% chance of collapsing.

But just the loss of a constant river of warmer water flowing toward Europe could lower temperatures there, strengthen hurricanes and raise the sea level along the northeastern coast of North America.

“You’re not transporting as much water, so it gets backed up along the East Coast,” Dutton said.

The ‘snow forest’ disappears

The vast boreal forests of the north face a future as treeless grasslands.

Cold weather forests that run across the Western United States, Canada and Alaska are estimated to store more than 30% of all forest carbon on the planet. Without them, huge amounts of greenhouse gases would be released into the atmosphere, worsening global warming.

A combination of three things are destroying it: heat, fire and bark beetles. Rising temperatures cause droughts and make forest fires more likely. Heat also boosts the population of bark beetles devastating the forests.

“Forests can tolerate heat and drought up to a point, and then there’s a point where they can’t tolerate anymore,” Swain said. “There’s evidence that we’re hitting that point or close to it.”

Bark beetles are native to North America. In northern latitudes, when winters are cold and summers cool, they typically reproduce once a year. With warmer and shorter winters, they can reproduce twice, resulting in larger populations and more stress and tree death.

The dead trees become fire hazards, causing wildfires to burn larger and hotter. When the fire is gone, grasslands, not forests, can grow back.

“There are some trees that are well adapted to the harsh cold, but you’ve made the summers too hot for them, so they’re replaced with a steppe grassland that can cope with the hotter summers,” Lenton said.

The time is now

Scientists and many of the world’s political leaders are unequivocal: The time for action is now. Not next year, not a decade from now.

“The stakes are clear. Complacency will be met by irreversible and unthinkable impacts from climate change,” John Kerry, the U.S. special presidential envoy for climate change, said Monday.

Any of these collapses, even if not total, would be bad for the planet, experts say. Even worse, as systems become unstable, they affect others, leading to more instability and potential collapse. Carbon currently stored in the earth would be released into the air, leading to more temperature rise and calamity.

In the face of these possibilities, it’s vital that humanity avoid increasing the planet’s temperature any more than it already has, experts say.

“We’re approaching thresholds we really don’t want to walk through,” Schlosser said. “We’re near the zone where the Earth is getting back at us.”

Researchers reveal variations in Arctic amplification effect during past millennium

The recent amplified warming in the Arctic during the last decades has received much attention. But how Arctic amplification (AA) has varied on longer time scales and what drives these variations remain unclear.

Recently, a study has provided a new perspective on the AA effect during the past millennium based on the best available paleoclimate data and novel data assimilation methods.

The study was published in Nature Communications on April 6. It was conducted by researchers from the Northwest Institute of Eco-Environment and Resources of the Chinese Academy of Sciences (CAS), the Institute of Tibetan Plateau Research of CAS, the Lund University and the University of Gothenburg.

The researchers produced a new millennium-long temperature reconstruction over the Northern Hemisphere by combining climate model simulations with newly available paleoclimate proxy records from the Past Global Changes 2k Network (PAGES2k) consortium, resulting in physically consistent and spatiotemporally continuous temperature fields.

Additionally, to quantify the variations in the strength of the AA, the researchers reconstructed a millennial AA index series, which revealed a significantly declining AA effect on the millennial time scale.

The millennial AA index series revealed that AA exhibited strong variations over a broad range of time scales, which can be explained, to a large part, by the phase of the Atlantic Multi-decadal Oscillation (AMO) and recent anthropogenic greenhouse gas forcing.

This result highlights the importance of the AMO and enhanced greenhouse effect in modulating AA, and suggests that there is predictability in AA on multi-decadal time scales.

The findings of this study may help fill the gaps in understanding the AA variation over the preindustrial era, improve the predictive ability of the Arctic and global climate change on the multi-decadal time scale, and distinguish the contributions of the natural variability of climate system and anthropogenic forcing to AA variation.

More information: Miao Fang et al, Arctic amplification modulated by Atlantic Multidecadal Oscillation and greenhouse forcing on multidecadal to century scales, Nature Communications (2022). DOI: 10.1038/s41467-022-29523-x
Journal information: Nature Communications
Provided by Chinese Academy of Sciences.

Dust storm covers Iraq for second time in a week

A dust storm blanketed Iraq again on Tuesday, sending people to hospital with breathing difficulties and leading airports to suspend flights.

It follows a similar storm that blew over the country late last week and left dozens hospitalised with respiratory problems.

The latest weather event cast an orange hue over the capital Baghdad, where it severely restricted visibility and coated buildings and cars in dust.

Pedestrians wore disposable masks to avoid inhaling the particles, AFP journalists said.

“People have been hospitalised with breathing difficulties, but most cases are minor,” health ministry spokesman Saif al-Badr told AFP.

Dozens of flights were suspended in Baghdad and the Shiite holy city of Najaf during the morning, before flights resumed in the afternoon when conditions improved, airport sources said.

While sand and dust storms are not uncommon during the Iraqi spring, they are expected to become even more frequent “due to drought, desertification and declining rainfall”, said the director of Iraq’s meteorological office, Amer al-Jabri.

Iraq is particularly vulnerable to climate change, with record low rainfall and high temperatures in recent years.

Experts have said these factors threaten social and economic disaster in the war-scarred country.

In November, the World Bank warned that Iraq could suffer a 20 percent drop in water resources by 2050 due to climate change.

New study confirms potential of geoelectrical methods in search for hidden graves

Rather than digging to identify unmarked mass grave sites or evidence to locate missing persons, cutting-edge technologies are helping law enforcement agents, forensic scientists and historians uncover attempts to hide victims.

New research by geophysicists at The University of Toledo published in the journal Forensic Science International validates the potential of methods called electrical resistivity and ground-penetrating radar as useful tools in the search for clandestine graves, with mass graves having a stronger and different “geophysical signature” compared to individual ones.

Related results of the research also are published in the journal Frontiers in Environmental Sciences.

“While the entire search process ultimately requires excavating shallow graves to retrieve human remains as evidence to prosecute suspects and bring closure to families of victims, engaging in such excavation without useful leads on the exact location of the graves will mean excavating large areas, which is difficult, time consuming and destructive,” said Dr. Kennedy Doro, assistant professor in the UToledo Department of Environmental Sciences and lead investigator of the study. “It also could lead to altering the target evidence.”

Using an innovative experiment design of mass and individual graves with human cadavers willingly donated for scientific research, researchers used ground-penetrating radar, electrical resistivity tomography and electromagnetic imaging from the surface before the burial through six months after the burial.

Helping direct the final excavation to more definite areas, researchers can provide an underground picture or geophysical signature to identify areas with unusual signals that may be related to excavation and human decay.

Electrical resistivity is a fundamental property of a material that measures how strongly it resists electrical current.

Through the study, researchers found that resistivity increases immediately after burial and decreases as time goes by.

Ground-penetrating radar shows the position of the graves and the human remains as disturbed and curved reflectors; however, it is limited by the presence of rock fragments distributed within the soil at the site where this study was carried out.

The experiment was established in May 2021 and consists of a mass grave with six human remains, three individual graves and two empty control graves dug to the same size as the mass grave and individual graves.

UToledo led the geophysical study in collaboration with other scientists from the University of Toronto and Linnaeus University and forensic anthropologists at Texas State University, which operates a 26-acre human decomposition and forensic taphonomy facility located at the Freeman Ranch in San Marcos.

“These initial results validate the capability of geoelectrical methods in detecting anomalies associated with disturbed ground and human decay, while ground-penetrating radar is limited by the geology of the site,” Doro said.

Before starting to dig the undisturbed ground, the team measured its electrical resistivity tomography, electromagnetics and ground-penetrating radar.

After excavating the land, the researchers analyzed soil profiles and added sensors at the grave sites to monitor changes in soil moisture, temperature and electrical conductivity.

“The availability of advanced tools and techniques with high accuracies, capable of covering a large investigation area within a short time without necessarily altering the target evidence, is crucial to the success of forensic investigative searches,” Doro said. “Most previous studies in this direction only assessed individual graves using pigs as proxies for humans. We used both individual and mass graves as well as human remains donated for science.”

More information: Kennedy O. Doro et al, Geophysical imaging of buried human remains in simulated mass and single graves: Experiment design and results from pre-burial to six months after burial, Forensic Science International (2022). DOI: 10.1016/j.forsciint.2022.111289
Time-lapse electrical resistivity tomography imaging of buried human remains in simulated mass and individual graves. Frontiers in Environmental Sciences. www.frontiersin.org/articles/1 … 2022.882496/abstract

Journal information: Forensic Science International
Provided by University of Toledo.

Understanding the Earth under Hawaii

In the 1960s, some 50 years after German researcher Alfred Wegener proposed his continental drift hypothesis, the theory of plate tectonics gave scientists a unifying framework for describing the large-scale motion of the surface plates that make up the Earth’s lithosphere—a framework that subsequently revolutionized the geosciences.

How those plates move around the Earth’s surface is controlled by motion within the mantle—the driving force of which is convection due to thermal anomalies, with compositional heterogeneity also expected. However, the technical challenge of visualizing structures inside an optically impenetrable, 6,371-kilometer-radius rock sphere has made understanding the compositional and thermal state of the mantle, as well as its dynamic evolution, a long-standing challenge in Earth science.

Now, in a paper published today in Nature Communications, researchers from MIT, Imperial College, Rice University, and the Institute of Earth Sciences in France report direct evidence for lateral variations in mantle composition below Hawaii. The results provide scientists with important new insights into how the Earth has evolved over its 4.5 billion year history, why it is as it is now, and what this means for rocky planets elsewhere.

Compositional variation

Scientists treat the mantle as two layers—the lower mantle and the upper mantle—separated by a boundary layer termed the mantle transition zone (MTZ). Physically, the MTZ is bounded by two seismic-velocity discontinuities near 410 km and 660 km depth (referred to as 410 and 660). These discontinuities, which are due to phase transitions in silicate minerals, play an important role in modulating mantle flow. Lateral variations in depth to these discontinuities have been widely used to infer thermal anomalies in the mantle, as mineral physics predicts a shallower 410 and a deeper 660 in cold regions and a deeper 410 and a shallower 660 in hot regions.

Previous petrological and numerical studies also predict compositional segregation of basaltic and harzburgitic material (and thus compositional heterogeneity) near the base of the MTZ in the relatively warm low-viscosity environments near mantle upwellings. But observational evidence for such a process has been scarce.

The new study, however, demonstrates clear evidence for lateral variation in composition near the base of the MTZ below Hawaii. This evidence could have important implications for our general understanding of mantle dynamics.https://googleads.g.doubleclick.net/pagead/ads?client=ca-pub-6900298817217782&output=html&h=280&adk=2862089727&adf=3688871403&pi=t.aa~a.3985241578~i.19~rp.4&w=696&fwrn=4&fwrnh=100&lmt=1649698477&num_ads=1&rafmt=1&armr=3&sem=mc&pwprc=6266171416&psa=1&ad_type=text_image&format=696×280&url=https%3A%2F%2Fwww.geologypage.com%2F2018%2F03%2Funderstanding-the-earth-under-hawaii.html&fwr=0&pra=3&rh=174&rw=696&rpe=1&resp_fmts=3&wgl=1&fa=27&adsid=ChAI8KPPkgYQuczCu-Kjjc9WEj0AtV76KIemBaSyb1BwcHJxD7GR6taoEeG6_zKJfSg0-VhOyZL_otlEs272-px95n7Rmwc9BsuKMvi_WikJ&uach=WyJXaW5kb3dzIiwiMTAuMC4wIiwieDg2IiwiIiwiMTAwLjAuNDg5Ni43NSIsW10sbnVsbCxudWxsLCI2NCIsW1siIE5vdCBBO0JyYW5kIiwiOTkuMC4wLjAiXSxbIkNocm9taXVtIiwiMTAwLjAuNDg5Ni43NSJdLFsiR29vZ2xlIENocm9tZSIsIjEwMC4wLjQ4OTYuNzUiXV0sZmFsc2Vd&tt_state=W3siaXNzdWVyT3JpZ2luIjoiaHR0cHM6Ly9wYWdlYWQyLmdvb2dsZXN5bmRpY2F0aW9uLmNvbSIsInN0YXRlIjoyOSwiaGFzUmVkZW1wdGlvblJlY29yZCI6dHJ1ZX1d&dt=1649698477567&bpp=4&bdt=3437&idt=-M&shv=r20220406&mjsv=m202203310101&ptt=9&saldr=aa&abxe=1&cookie=ID%3Dd99587530b7b1bb3-2271c2e674cd003d%3AT%3D1649694190%3ART%3D1649694190%3AS%3DALNI_MatOH9vwhGpvCeyaWAs8nKWqzEnpw&prev_fmts=728×90%2C728x90%2C336x280%2C300x600%2C0x0%2C696x280&nras=3&correlator=1452444588971&frm=20&pv=1&ga_vid=2080888841.1649694190&ga_sid=1649698476&ga_hid=1505154551&ga_fc=1&ga_cid=1633490170.1649694191&u_tz=120&u_his=2&u_h=768&u_w=1366&u_ah=728&u_aw=1366&u_cd=24&u_sd=1&dmc=8&adx=141&ady=2294&biw=1349&bih=625&scr_x=0&scr_y=0&eid=44759875%2C44759926%2C44759837%2C31066932%2C21067496&oid=2&pvsid=1566347715824853&pem=579&tmod=1176839909&uas=3&nvt=1&ref=https%3A%2F%2Fwww.geologypage.com%2F2020%2F06%2Fscientists-detect-unexpected-widespread-structures-near-earths-core.html&eae=0&fc=384&brdim=0%2C0%2C0%2C0%2C1366%2C0%2C1366%2C728%2C1366%2C625&vis=1&rsz=%7C%7Cs%7C&abl=NS&fu=128&bc=31&jar=2022-04-11-15&ifi=9&uci=a!9&btvi=4&fsb=1&xpc=BXucA5jT0j&p=https%3A//www.geologypage.com&dtd=118

As lead author Chunquan Yu Ph.D. ’16, a former grad student in the Hilst Group at MIT who is now a postdoc at Caltech, explains, “At middle ocean ridges, plate separation results in ascending and partial melting of the mantle material. Such a process causes differentiation of the oceanic lithosphere with basaltic material in the crust and harzburgitic residue in the mantle. As the differentiated oceanic lithosphere cools, it descends back into the mantle along the subduction zone. Basalt and harzburgite are difficult to separate in cold environments. However, they can segregate in relative warm low-viscosity environments, such as near mantle upwellings, potentially providing a major source of compositional heterogeneity in the Earth’s mantle.”

Looking with earthquakes

To explore this idea, Yu and his colleagues used a seismic technique involving the analysis of underside shear wave reflections off mantle discontinuities—known as SS precursors—to study MTZ structures beneath the Pacific Ocean around Hawaii.

“When an earthquake occurs, it radiates both compressional (P) and shear wave (S) energy. Both P and S waves can reflect from interfaces in the Earth’s interior,” Yu explains. “If an S wave leaves a source downward and reflects at the free surface before arriving at the receiver, it is termed SS. SS precursors are underside S-wave reflections off mantle discontinuities. Because they travel along shorter ray paths, they are precursory to SS.”

Using a novel seismic array technique, the team were able to improve the signal-to-noise ratio of the SS precursors and remove interfering phases. As a result, much more data that otherwise would have been discarded became accessible for analysis.

They also employed so-called amplitude versus offset analysis, a tool widely used in exploration seismology, to constrain elastic properties near MTZ discontinuities.

The analysis finds strong lateral variations in radial contrasts in mass density and wavespeed across 660 while no such variations were observed along the 410. Complementing this, the team’s thermodynamic modeling, along a range of mantle temperatures for several representative mantle compositions, precludes a thermal origin for the inferred lateral variations in elastic contrasts across 660. Instead, the inferred 660 contrasts can be explained by lateral variation in mantle composition: from average (pyrolytic; about 60 percent olivine) mantle beneath Hawaii to a mixture with more melt-depleted harzburgite (about 80 percent olivine) southeast of the hotspot. Such compositional heterogeneity is consistent with numerical predictions that segregation of basaltic and harzburgitic material could occur near the base of the MTZ near hot deep mantle upwellings like the one that is often invoked to cause volcanic activity on Hawaii.

“It has been suggested that compositional segregation between basaltic and harzburgitic materials could form a gravitationally stable layer over the base of the MTZ. If so it can provide a filter for slab downwellings and lower-mantle upwellings, and thus strongly affect the mode of mantle convection and its chemical circulation,” says Yu.

This study presents a promising technique to get constraints on the thus far elusive distribution of compositional heterogeneity within Earth’s mantle. Compositional segregation near the base of the MTZ has been expected since the 1960s and evidence that this process does indeed occur has important implications for our understanding of the chemical evolution of the Earth.

Reference:
“Compositional heterogeneity near the base of the mantle transition zone beneath Hawaii” Nature Communications (2018). DOI: 10.1038/s41467-018-03654-6.

Scientists detect unexpected widespread structures near Earth’s core

University of Maryland geophysicists analyzed thousands of recordings of seismic waves, sound waves traveling through the Earth, to identify echoes from the boundary between Earth’s molten core and the solid mantle layer above it. The echoes revealed more widespread, heterogenous structures — areas of unusually dense, hot rock — at the core-mantle boundary than previously known.

Scientists are unsure of the composition of these structures, and previous studies have provided only a limited view of them. Better understanding their shape and extent can help reveal the geologic processes happening deep inside Earth. This knowledge may provide clues to the workings of plate tectonics and the evolution of our planet.

The new research provides the first comprehensive view of the core-mantle boundary over a wide area with such detailed resolution. The study was published in the June 12, 2020, issue of the journal Science.

The researchers focused on echoes of seismic waves traveling beneath the Pacific Ocean basin. Their analysis revealed a previously unknown structure beneath the volcanic Marquesas Islands in the South Pacific and showed that the structure beneath the Hawaiian Islands is much larger than previously known.

“By looking at thousands of core-mantle boundary echoes at once, instead of focusing on a few at a time, as is usually done, we have gotten a totally new perspective,” said Doyeon Kim, a postdoctoral fellow in the UMD Department of Geology and the lead author of the paper. “This is showing us that the core-mantle boundary region has lots of structures that can produce these echoes, and that was something we didn’t realize before because we only had a narrow view.”

Earthquakes generate seismic waves below Earth’s surface that travel thousands of miles. When the waves encounter changes in rock density, temperature or composition, they change speed, bend or scatter, producing echoes that can be detected. Echoes from nearby structures arrive more quickly, while those from larger structures are louder. By measuring the travel time and amplitude of these echoes as they arrive at seismometers in different locations, scientists can develop models of the physical properties of rock hidden below the surface. This process is similar to the way bats echolocate to map their environment.

For this study, Kim and his colleagues looked for echoes generated by a specific type of wave, called a shear wave, as it travels along the core-mantle boundary. In a recording from a single earthquake, known as a seismogram, echoes from diffracted shear waves can be hard to distinguish from random noise. But looking at many seismograms from many earthquakes at once can reveal similarities and patterns that identify the echoes hidden in the data.

Using a machine learning algorithm called Sequencer, the researchers analyzed 7,000 seismograms from hundreds of earthquakes of 6.5 magnitude and greater occurring around the Pacific Ocean basin from 1990 to 2018. Sequencer was developed by the new study’s co-authors from Johns Hopkins University and Tel Aviv University to find patterns in radiation from distant stars and galaxies. When applied to seismograms from earthquakes, the algorithm discovered a large number of shear wave echoes.

“Machine learning in earth science is growing rapidly and a method like Sequencer allows us to be able to systematically detect seismic echoes and get new insights into the structures at the base of the mantle, which have remained largely enigmatic,” Kim said.

The study revealed a few surprises in the structure of the core-mantle boundary.

“We found echoes on about 40% of all seismic wave paths,” said Vedran Lekić, an associate professor of geology at UMD and a co-author of the study. “That was surprising because we were expecting them to be more rare, and what that means is the anomalous structures at the core-mantle boundary are much more widespread than previously thought.”

The scientists found that the large patch of very dense, hot material at the core-mantle boundary beneath Hawaii produced uniquely loud echoes, indicating that it is even larger than previous estimates. Known as ultralow-velocity zones (ULVZs), such patches are found at the roots of volcanic plumes, where hot rock rises from the core-mantle boundary region to produce volcanic islands. The ULVZ beneath Hawaii is the largest known.

This study also found a previously unknown ULVZ beneath the Marquesas Islands.

“We were surprised to find such a big feature beneath the Marquesas Islands that we didn’t even know existed before,” Lekić said. “This is really exciting, because it shows how the Sequencer algorithm can help us to contextualize seismogram data across the globe in a way we couldn’t before.”

Reference:
D. Kim, V. Lekić, B. Ménard, D. Baron and M. Taghizadeh-Popp. Sequencing Seismograms: A Panoptic View of Scattering in the Core-Mantle Boundary Region. Science, 2020 DOI: 10.1126/science.aba8972

Paleogene Period

The Paleogene is a geologic period and system that began 66 and ended 23.03 million years ago and comprises the first part of the Cenozoic Era. Lasting 43 million years, the Paleogene is most notable as being the time in which mammals evolved from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding Cretaceous Period.
This period consists of the Paleocene, Eocene, and Oligocene Epochs. The end of the Paleocene (55.5/54.8 Mya) was marked by one of the most significant periods of global change during the Cenozoic, the Paleocene-Eocene Thermal Maximum, which upset oceanic and atmospheric circulation and led to the extinction of numerous deep-sea benthic foraminifera and on land, a major turnover in mammals.

The Paleogene follows the Cretaceous Period and is followed by the Miocene Epoch of the Neogene Period. The terms ‘Paleogene System’ (formal) and ‘lower Tertiary System’ (informal) are applied to the rocks deposited during the ‘Paleogene Period’. The somewhat confusing terminology seems to be due to attempts to deal with the comparatively fine subdivisions of time possible in the relatively recent geologic past, when more information is preserved. By dividing the Tertiary Period into two periods instead of directly into five epochs, the periods are more closely comparable to the duration of ‘periods’ in the Mesozoic and Paleozoic Eras.

Climate and geography

The global climate during the Paleogene departed from the hot and humid conditions of the late Mesozoic era and began a cooling and drying trend which, although having been periodically disrupted by warm periods such as the Paleocene–Eocene Thermal Maximum, persists today. The trend was partly caused by the formation of the Antarctic Circumpolar Current, which significantly cooled oceanic water temperatures.The continents during the Paleogene continued to drift closer to their current positions. India was in the process of colliding with Asia, subsequently forming the Himalayas.

The Atlantic Ocean continued to widen by a few centimeters each year. Africa was moving north to meet with Europe and form the Mediterranean, while South America was moving closer to North America (they would later connect via the Isthmus of Panama). Inland seas retreated from North America early in the period. Australia had also separated from Antarctica and was drifting towards Southeast Asia.

Flora and fauna

Scene featuring typical Eocene (Mid-Paleogene) flora and fauna © Jay Matternes

Mammals began a rapid diversification during this period. After the Cretaceous–Paleogene extinction event, which saw the demise of the non-avian dinosaurs, they transformed from a few small and generalized forms and began to evolve into most of the modern varieties we see today. Some of these mammals would evolve into large forms that would dominate the land, while others would become capable of living in marine, specialized terrestrial, and airborne environments.

Some mammals took to the oceans and became modern cetaceans, while others took to the trees and became primates, the group to which humans belong. Birds, which were already well established by the end of the Cretaceous, also experienced an adaptive radiation as they took over the skies left empty by the now extinct Pterosaurs. Most other branches of life remained relatively unchanged in comparison to birds and mammals during this period.

As the Earth began to cool, tropical plants were less numerous and were now restricted to equatorial regions. Deciduous plants became more common, which could survive through the seasonal climate the world was now experiencing. One of the most notable floral developments during this period was the evolution of the first grass species. This new plant type expanded and formed new ecological environments we know today as savannas and prairies. These grasslands also began to replace many forests because they could survive better in the drier climate typical in many regions of the world during this period.

Geology

The Paleogene is notable in the context of offshore oil drilling, and especially in Gulf of Mexico oil exploration, where it is usually referred to as the “Lower Tertiary”. These rock formations represent the current cutting edge of deep-water oil discovery.Lower Tertiary rock formations encountered in the Gulf of Mexico oil industry tend to be comparatively high temperature and high pressure reservoirs, often with high sand content (70%+) or under very thick salt sediment layers.

Early Earth’s atmosphere was less conducive to lightning

In 1952, Stanley Miller and Harold Urey made sparks fly in a gas-filled flask meant to reflect the composition of Earth’s atmosphere around 3.8 billion years ago. Their results suggested that lightning could have led to prebiotic molecules necessary for the evolution of life, such as amino acids. At the time, scientists thought the early atmosphere would have been primarily methane and ammonia, but by the 1990s, experts argued for an atmosphere filled with carbon dioxide and molecular nitrogen.

Now, a new study suggests that the composition of Earth’s primordial atmosphere likely made it harder to generate lightning, which may have increased the time it took to generate and accumulate prebiotic molecules important for life.

Lightning Behavior in Different Atmospheric Compositions

Electrons behave differently in an atmosphere composed of methane and ammonia versus one made mostly of carbon dioxide and molecular nitrogen. It stands to reason lightning discharges would behave differently, too, which could affect the likelihood of prebiotic molecules forming on early Earth. Yet few people have modeled how lightning discharges vary in different atmospheric environments.

To look at how often electrons and gas molecules would have collided in the two versions of early Earth atmospheres, Köhn et al. modeled the probability of discharge sparking—the first step to a lightning strike. They found that in the carbon dioxide–nitrogen atmosphere, it’s harder to get lightning to spark.

“Basically, in the nitrogen- and carbon-rich atmosphere, you need stronger electric fields for a discharge to initiate,” said Christoph Köhn, a scientist at the National Space Institute at the Technical University of Denmark, who led the study.

The models revealed that the carbon dioxide and nitrogen atmosphere needed about a 28% stronger electric field for streamers—the precursors of lightning—to discharge, because gas molecules and electrons are less likely to collide and build up electrical charges that can generate lightning strikes. Scaling up over space and time suggests there may have been fewer lightning strikes early in Earth’s history, therefore shrinking the odds of generating prebiotic molecules.

“If lightning discharges were responsible for the production of prebiotic molecules, it’s important to get a very good theoretical understanding of what happened,” said Köhn. “The big question is still, Where do all these prebiotic molecules come from?”

The study strictly modeled the earliest stages of a lightning strike—the sparks that start strikes—so for Köhn and colleagues, the next steps are to model whole lightning strikes and couple that with models of atmospheric chemistry. Together these studies could give a more complete look into how lightning may have been linked to prebiotic molecules.

More information: Rebecca Dzombak, Lightning Had Difficulty Forming in Early Earth’s Atmosphere, Eos (2022). DOI: 10.1029/2022EO220187 C. Köhn et al, Streamer Discharges in the Atmosphere of Primordial Earth, Geophysical Research Letters (2022). DOI: 10.1029/2021GL097504
Journal information: Geophysical Research Letters
Provided by American Geophysical Union.

Aftershocks of 1959 earthquake rocked Yellowstone in 2017-18

On Aug. 17, 1959, back when Dwight D. Eisenhower was president, the U.S. had yet to send a human to space and the nation’s flag sported 49 stars, Yellowstone National Park shook violently for about 30 seconds. The shock was strong enough to drop the ground a full 20 feet in some places. It toppled the dining room fireplace in the Old Faithful Inn. Groundwater swelled up and down in wells as far away as Hawaii. Twenty-eight people died. It went down in Yellowstone history as the Hebgen Lake earthquake, with a magnitude of 7.2.

And in 2017, nearly 60 years and 11 presidents later, the Hebgen Lake quake shook Yellowstone again. A swarm of more than 3,000 small earthquakes in the Maple Creek area (in Yellowstone National Park but outside of the Yellowstone volcano caldera) between June 2017 and March 2018 are, at least in part, aftershocks of the 1959 quake. That’s according to a study published in Geophysical Research Letters by University of Utah geoscientists led by Guanning Pang and Keith Koper.

“These kinds of earthquakes in Yellowstone are very common,” says Koper, director of the University of Utah Seismograph Stations. “These swarms happen very frequently. This one was a little bit longer and had more events than normal.”

“We don’t think it will increase the risk of an eruption,” Pang adds.