Plants grown in simulated lunar soil on the left and in Apollo sample on the right, seen 16 days after planting.
Credit: Tyler Jones, UF/IFAS

Well, not exactly. Scientists recently grew plants in lunar soil for the first time in history. The lunar soil, also called moon dust, was brought back from three Apollo missions. Scientists from the University of Florida planted thale cress in the moon dust and compared the growth to materials found on Earth’s surface, such as volcanic ash. Thale cress is a small, bitter-tasting plant similar to broccoli, cauliflower, and kale. After two days, the seeds had germinated (grown). However, the plants in moon soil did not thrive compared to the plants in Earth soil after six days.

Lunar soil is very different from the soil on Earth. Soil is the mixture of minerals, organic matter, and other materials that covers most of Earth’s land. Soil is a storehouse of nutrients and the decayed remains of organisms (living things). Lunar soil is more dusty and is not made up of decayed organisms, so it does not contain as many nutrients compared to soil found on Earth. Impacts of micrometeoroids (tiny meteoroids‘) grind the surface rocks into a fine, dusty powder known as regolith. Regolith overlies all the bedrock on the moon. Because regolith forms as a result of exposure to space, the longer a rock is exposed, the thicker the regolith that forms on it.

National Aeronautics and Space Association (NASA) granted the scientists 12 grams of lunar soil for the experiment because it is precious and cannot be wasted. The soil brought back from Apollo 11 was not as strong as the soil brought back from Apollo 12 and 17. The scientists believe soil from Apollo 11 was damaged by cosmic rays and radiation from solar wind on the moon’s surface. Scientists have already started planning where they could find better moon soil where lava flow has enriched the soil.

For years, scientists have wondered whether the moon could support life. If humans were to survive on the moon permanently, they would need to grow plants for food. Although the experiment did not prove that the moon could sustain life, it gives hope that there could be vegetation on the moon someday. We are one step closer to growing an herb garden on the moon!

A particle detector helps scientists study subatomic particles. Physicists at the Fermi National Accelerator Laboratory in Batavia, Ill., use this detector to record information about particles produced in collisions between beams of protons and beams of antiprotons.
Credit: Fermilab Visual Media Services

Particle physicists are buzzing about a hefty discovery. In April 2022, researchers at the Fermi National Accelerator Laboratory (also known as Fermilab) announced that a particle called the W boson appears to have slightly more mass than expected. Their results were published in the journal Science.

Bosons are particles that transmit forces between other particles. As particles go, bosons are much less popular than their cousins the fermions, which make up matter. The W boson carries the weak nuclear force, which is involved in the decay (breakdown) of some radioactive atoms.

A particle accelerator helps scientists study electricity and the building blocks of matter. The accelerator at the Fermi National Accelerator Laboratory in Batavia, Illinois, accelerates protons to almost the speed of light in an underground tunnel, shown here.
Credit: Fermi National Accelerator Laboratory

So who cares about a chunky boson? Physicists do. Modern physics is based largely on a theory called the Standard Model. The Standard Model includes a family tree of particles and can be used to make predictions about their properties. Most of these predictions have turned out to be highly accurate. A deviation in the mass of the W boson, if confirmed, could hint at the existence of unknown particles or other revisions to the Standard Model.

Physicists study particles in giant devices called particle accelerators. As the name suggests, these devices accelerate particles to extremely high speeds. They then smash them together to study any particles created in the collision.

The experiments in question were conducted in an accelerator called the Tevatron. The device smashed positively charged particles called protons into anti-protons, their antimatter counterparts. About one in 10 million such collisions create a W boson. It took the scientists 10 years to collect enough data.

The Tevatron was shut down in 2011. But it took another 10 years to properly analyze all that data. The results suggest that the W boson is 0.1 percent heavier than expected. That’s about as much as your weight might vary if measured before and after lunch. But for extremely precise particle measurements, it may be just enough to alter our understanding of the universe.

Brontosaurus.
Credit: © Emiliano Troco

Sauropods were the most spectacular of the dinosaurs. Their long necks supported small heads that took in needles and leaves. Despite such a nutrient-poor diet, they reached sizes and lengths unparalleled in any other terrestrial (land-dwelling) animals. How—and why—did they get so large? A recent study may have discovered a lead to unraveling the physiology of these amazing animals. 

Over tens of millions of years, the arrangement of the continents has shifted through the action of plate tectonics. Geologists can trace how a location has moved over the face of Earth to determine its paleolatitude. The paleolatitude is the position of a point on the Earth’s surface in relation to the equator at a time in the distant past. Both latitude and paleolatitude are measured on a scale of 0° (the equator) to 90° (the poles). Higher latitudes experience cooler temperatures and less sunlight in winter. 

Dinosaurs reigned during the Mesozoic Era—a time of warmer climates. Despite the planet being largely ice-free, regions near the poles still faced cold winters and weeks or months without sunlight. Nevertheless, dinosaurs have been found at high paleolatitudes, including in Antarctica and Alaska. At least some of these dinosaurs remained there through the winter. 

Sauropod fossils, however, are conspicuously absent from these polar locations. No sauropod fossil has been discovered from a paleolatitude higher than about 65°. Instead, these chilly climates were strictly occupied by meat-eating theropods and some plant-eating dinosaurs called ornithischians. 

Some paleontologists (scientists who study prehistoric life) suspected the absence of fossils suggest that sauropods preferred warmer climates. But others thought that sauropods might not have fossilized well near the poles for some reason, or that the fossils are still waiting to be discovered. 

A team led by Alfio Alessandro Chiarenza of the University of Vigo in Spain analyzed the paleolatitude of all the places where sauropod fossils have been found. The team published their findings last month in the scientific journal Current Biology. They determined that the absence of sauropods at high paleolatitudes was not due to incomplete sampling. Chiarenza’s team used models of the Mesozoic climate and found that sauropods preferred savanna-type habitats. Sauropod ranges were tightly constrained by the lowest predicted temperature. 

Why didn’t (or couldn’t) sauropods brave the cold? They might have cooled down too quickly, despite their massive sizes. Many theropods—and possibly some ornithischians—had downy or hairlike feathers that could be used to keep them warm. Sauropods lacked any such insulation. Furthermore, a sauropod’s long necks and tails might have lost heat quickly when exposed to bitter-cold winds. 

Sauropods buried their eggs in the earth to keep them at a stable temperature. But this method probably would not have kept the eggs warm enough in cold climates. In contrast, theropods sat on their eggs and ornithischians covered their eggs in rotting plants. Both of these approaches could keep the eggs warm even in cold climates. 

Chiarenza’s team proposes that sauropods did not possess as high of a metabolism as theropods and ornithischians. Historically, scientists have classified animals as endothermic (“warm-blooded”) or ectothermic (“cold-blooded”). Endothermic animals tend to produce more of their own body heat, while ectothermic animals tend to rely more on their environment for heat. This is a false division, since every animal is somewhat reliant on its environment for heat. But animals classified as endothermic can usually survive in cooler temperatures. Reptiles, the classic endotherms, are concentrated near the equator. 

In many ways, this makes a lot of sense. A lower metabolism would have enabled sauropods to survive on less food. Their huge size would cause them to lose less heat to their environment, much like a well-insulated building. Growing evidence suggests that the ancestor of dinosaurs and crocodilians (a group of reptiles) had a high metabolism, but crocodilians “slowed down” when dinosaurs took over most environmental niches. A similar changed might have occurred in sauropods as well, enabling them to attain colossal sizes. Sometimes slow and steady wins the race. 

Surgeons performed an eight-hour procedure to transplant a genetically modified pig’s heart into a human on Jan. 7.
Credit: University of Maryland School of Medicine

For the first time ever, surgeons at the University of Maryland Medical Center successfully transplanted a heart from a genetically modified pig to a human. The eight-hour surgery took place on Jan. 7, 2022, in Baltimore, Maryland. The recipient was a 57-year-old man with heart disease, called arrhythmia. He was deemed too sick to receive a human heart. Scientists had altered the genes of the pig to make it more similar to humans, removing four pig genes and adding six human genes through genetic engineering.

More than 107,000 people are on waiting lists to receive organ donations in the United States. Transplanted tissues and organs replace diseased, damaged, or destroyed body parts. They can help restore the health of a person who might otherwise die or be seriously disabled. Commonly transplanted organs include the heart, lungs, kidney, and liver.

Because of the shortage of human organs, researchers are actively investigating the use of donor organs from animals. Transplanting organs from one species to another is called xenotransplantation. Use of pigs as organ donors is an especially active area of research. Pigs are already widely raised for food and leather, and their organs are about the same size as adult human organs. One major concern is preventing accidental transfer of viruses from other animals to people. Another challenge is preventing the recipient’s immune system from destroying a donor organ. If the immune system recognizes that a transplanted organ came from outside the body, the system attacks the organ as a dangerous invader. This reaction is called rejection. Doctors try to prevent rejection by choosing the best donor and prescribing immunosuppressive drugs, which are special medications to protect the transplant.

Xenotransplantation has been studied for over 60 years but is not authorized in the United States. The process of raising genetically modified animals to harvest their organs is widely debated. The Food and Drug Administration gave the surgery team an emergency authorization on Dec. 31, 2021, to conduct the transplant due to the recipient’s condition.

From the long list of people waiting to receive a lifesaving organ, 17 people die each day. This groundbreaking surgery is giving hope to many patients and their family members who are waiting on organs. However, many surgeons and experts believe it is too early to call this xenotransplantation a success.

Kenyan-born paleoanthropologist Richard Leakey and his team discovered many prehistoric human fossils at Lake Turkana, Kenya. In this photograph, he is holding near-complete fossil skulls of Homo erectus, left, and Homo habilis, right.
Credit: © Chip Hires, Gamma-Rapho/Getty Images

Famed scientist, conservationist, and politician Richard Leakey passed away aged 77 on Jan. 2, 2022 at his home outside Nairobi, Kenya. The remarkable fossils of prehistoric human ancestors discovered by Leakey and his colleagues firmly established the origins of humanity in Africa.  

Richard Erskine Frere Leakey was born on Dec. 19, 1944 in Nairobi. He was the son of distinguished British anthropologists Louis and Mary Leakey, whose excavations at Olduvai Gorge in northern Tanzania uncovered fossils of an early human ancestor they named Homo habilis. Louis Leakey argued that Homo habilis was one of the earliest types of human beings. Other scientists were skeptical, thinking that our own species likely originated in other regions.  

As a child, Richard grew up at excavation sites in Olduvai Gorge run by his parents. As a rebellious teen, however, Richard Leakey was determined to stay out of the “family business” of searching for fossils of early human ancestors. He dropped out of school and worked for a time leading safaris. While flying his own airplane over a region of northern Kenya around Lake Turkana, he recognized landscapes that likely held abundant fossils. Leading his own team of fossil hunters, Richard discovered several fossils of human ancestors, including a nearly complete skull that he recognized as Homo habilis. This species is now considered by most anthropologists to be one of the earliest types of human beings. Homo habilis lived in Africa about 2 million years ago. 

In 1984, a member of Leakey’s team, Kamoya Kimeu, found an almost complete skeleton of a young man at a site called Nariokotome near Lake Turkana that dates about 1.6 million years ago. The skeleton was classified in the species Homo erectus, a prehistoric human ancestor known from fossils first discovered in the 1800’s in Asia and later in Europe. The well-preserved fossil skeleton demonstrates that Homo erectus had a larger brain compared to Homo habilis, and first appeared in Africa. The more intelligent Homo erectus was able to adapt to new environments and migrate out of the ancestral African homeland.  

From 1968 to 1989, Richard directed the National Museums of Kenya while he and his team continued fieldwork in the Lake Turkana region, discovering many important fossils of human ancestors. From 1990 to 1994, and briefly again in 1998, he headed the Kenya Wildlife Service (KWS). In that position, he worked to eliminate the illegal killing of Kenyan elephants for their tusks, a source of ivory. In 1995, Leakey helped found a Kenyan political party called Safina, to challenge the ruling Kenya African National Union (Kanu) party.  

Since 2002, Leakey has been a professor of anthropology at the State University of New York at Stony Brook. There, he led the Turkana Basin Institute responsible for continuing fieldwork in the Lake Turkana region. In 2004 he founded the conservation organization WildlifeDirect and also returned as head of the KWS from 2015 until 2018. 

An artist’s im­pres­sion of Plan­et GJ 367b.
Credit: SPP 1992 (Patricia Klein)

Do you know someone who listens to heavy metal music? Maybe you have friends who like to wear black clothing and bang their heads to loud tunes. Perhaps you have an uncle who’s into Ozzy Osbourne or Van Halen. You may know someone who’s pretty metal, but that person is probably an absolute creampuff compared with the heavy metal planet recently discovered by German scientists.

The planet, designated GJ367b, is an exoplanet, a planet orbiting a star beyond our solar system. It orbits a red dwarf star some 31 light-years from Earth in the southern constellation Vela, the Sails. One light-year is this distance light travels in one year, about 5.88 trillion miles (9.46 trillion kilometers).

At about 3/4 the size of Earth, GJ367b is the smallest exoplanet yet discovered. But, that does not mean that it is a lightweight. The exoplanet has a density of 8 grams per cubic centimeter, compared with about 5.5  grams per cubic centimeter for Earth. This extreme density suggests that GJ367b is the most metallic planet yet discovered. It probably consists mostly of an iron core, perhaps surrounded by a thin layer of rock.

The planet’s density is not its only extreme characteristic. The planet orbits extremely close to its parent star, whipping around the red dwarf every eight hours. If you lived on GJ367b, you might be able to celebrate your birthday about three times each Earth day. You probably wouldn’t like the weather, though. Daytime temperatures reach a sizzling 1500 °C (2700 °F). That’s almost hot enough to melt the planet’s metal. In fact, GJ367b may have an atmosphere composed of evaporated rock.

That scientists were able to learn so much about such a small planet shows just how far the hunt for exoplanets has advanced. Scientists discovered GJ367b using the Transiting Exoplanet Sky Survey (TESS) telescope, announcing the discovery in December. The TESS telescope identifies exoplanets by measuring changes in a star’s light as an orbiting planet transits (passes in front of) it. Scientists hope to learn even more about this heavy metal world with the launch of the James Webb Space Telescope.

Female California condors, an endangered species, are able to reproduce without male partners, in a process known as parthenogenesis.
© Claudio Contreras, Nature Picture Library

Even after years of study, the California condor is still surprising researchers. Recently, two of the giant birds were discovered to have been born through parthenogenesis, a form of reproduction in which an unfertilized egg still hatches. Parthenogenesis is a type of asexual reproduction. Human beings and almost all other animals reproduce sexually, through mating between a male and a female. In asexual reproduction, a new organism (living thing) develops from parts of, or parts produced by, one organism. This example of parthenogenesis is particularly noteworthy because the condor is a critically endangered species. At its lowest population in 1982, only around 20 California condors were alive, in the wild and in captivity.

In 1982, researchers launched a program to save the condors, and over the next few decades, the population grew to over 500. The researchers also studied the condors in captivity. They were able to collect DNA samples from feathers and eggshells and could pay close attention to the birds’ reproductive habits. They discovered that two of the male condors did not have any genetic indication of having been fathered by the other condors in captivity. Despite having only one parent, the condors were not clones (genetically identical copies) of the mother. Rather, through fusion between the unfertilized egg and another reproductive cell in the mother’s body, the offspring end up with a unique mixture of the mother’s genetic material. Female condors can only produce male offspring through parthenogenesis, due to the way sex is determined by chromosomes among birds.

While parthenogenesis is fairly rare, it is not unheard of, even in birds. Some species of turkey and domestic pigeons also have been known to reproduce in this way. Additionally, birds are far from the only animals that can undergo parthenogenesis. Parthenogenesis has been seen in species of sharks—including the hammerhead and bamboo shark—as well as some species of snakes and lizards. Some insects, like aphids and stick insects, can also reproduce asexually. However, parthenogenesis has not been documented in mammals.

Most scientists thought that parthenogenesis only happened in populations that lacked males. For example, a female shark recently surprisingly gave birth after living 10 years in an Italian aquarium where no male sharks were kept. But the female condors had males in captivity with them. Other female condors nested and produced chicks after mating with the local males.

California condors are the largest flying land birds in North America, with a wingspan of 8 to 9 1/2 feet (2.4 to 2.9 meters). They weigh up to 23 pounds (10.4 kilograms). In the wild, condors spend much of the day resting on high perches. Condors do not build nests. Instead, their eggs are laid in caves, in holes, or among boulders. A female California condor lays just one egg every two years. Condors are powerful, graceful fliers. They can soar and glide for long distances, flapping their wings an average of only once an hour. They may search the ground for food as they fly. Like other vultures, condors eat the remains of dead animals.

The growth of urban areas has posed a major threat to condor survival. The condor’s way of life requires vast areas of open, hilly country, and urban growth destroys such habitat.

An image captured by the GOES-16 satellite shows a flash (purple) most likely caused by a bolide (exploding meteor) over New Hampshire on Oct. 10, 2021.
Credit: NOAA

A mysterious boom rattled houses, shook the ground, and frightened pets in southern New Hampshire around 11:30 a.m. on Sunday, October 10. Curious people in the Granite State took to the internet to find the cause. Was it an earthquake, an aircraft, a single thunderclap, a spaceship, or a meteor? There was nothing in the news about it, so one observer called the fire department, which also did not have any answers. Around 400 residents shared their observations on volcanodiscovery.com, an online forum where people report seismic activity (vibrations from earthquakes). What caused the boom?

While earthquakes do occur in the area of New Hampshire, the United States Geological Survey announced that there were no earthquakes in all New England on Sunday. The Geological Survey is a federal agency tasked in part with monitoring such hazards as earthquakes and volcanoes.

Ruling out an earthquake, many people kept researching. One cause of confusion was that even though there was an audible (able to be heard) boom and physical thud, there was no damage reported. Was it a powerful military plane? The Federal Aviation Administration announced there was no unusual military flight activity over the state. One concerned resident theorized that the sound came from the recently established New Boston Space Force Station, previously an air force base.

Meteorologists said the mystery blast was most likely a sonic boom caused by a meteor. A meteor appears when a piece of matter enters Earth’s atmosphere from space at high speed, causing it to heat up. A fireball is a meteor that burns brightly as it plunges through the atmosphere. If the fireball explodes at the end of its path, it is called a bolide.

Greg Cornwell, a meteorologist for the National Weather Service, said that a suspicious spot appeared in images from the weather satellite GOES-16, which in part maps lightning strikes, around the same time people reported the boom. Weather satellite images generally pick up storms and other weather patterns. Although it was overcast that morning, there were no thunderstorms to explain the blip. Bolides and fireballs have in the past appeared as false storms in satellite images. Cornwell also explained that this time of year is known for meteor showers.

Many experts considered it likely that a meteor explosion produced the mysterious boom. However, to officially pin the blast on a meteor, scientists need a direct eyewitness account or video evidence. No solid eyewitness account or video evidence has been brought forward, so residents may have to settle for a hunch.

Sandra Lindsay, left, an African American nurse, is injected with the COVID-19 vaccine developed by Pfizer on Dec. 14, 2020, in the Queens borough (section) of New York City. The rollout of the vaccine, the first to be given emergency authorization by the Food and Drug Administration, began the biggest vaccination effort in U.S. history.
Credit: © Mark Lennihan, Getty Images

On Monday, Aug. 23, 2021, the United States Food and Drug Administration (FDA) fully approved the two-dose Pfizer vaccine for COVID-19. The FDA has granted full approval of the vaccine for those aged 16 years and older. Full approval of a vaccine will make it easier for public and private organizations to require vaccinations. This includes hospitals, active-duty military, and schools.

The coronavirus disease COVID-19 has killed more than 4 million people and infected more than 200 million people around the world. The first countries with access to a vaccine began vaccinating their citizens in December 2020. Almost 5 billion doses of a vaccine preventing COVID-19 have been administered to people around the world.

In late November 2020, the companies Pfizer and Moderna each applied for emergency approval from the FDA for their COVID-19 vaccines. The two companies are among dozens of drugmakers that worked tirelessly to develop a vaccine against the deadly virus. Because the vaccine was authorized for emergency use after a clinical trial of 40,000 people, many citizens were hesitant to receive the vaccine. Full approval of the vaccine may assure some of those yet to get the shot of the vaccine’s safety.

Pfizer and Moderna began clinical trials in July. During these trials, participants were given either the vaccine or a placebo. A placebo is a substance that contains no active ingredient. Comparing infection rates in subjects who received the placebo with those among subjects who got the vaccine can help determine if the vaccine is effective. In the Pfizer and Moderna clinical trials, half the participants were given a placebo of saltwater, and half were given the vaccine. The researchers then waited to see who might get sick. The results were very promising—both vaccines were about 95 percent effective in preventing COVID-19. By contrast, commonly administered influenza vaccines (known as flu shots) are 40 percent to 60 percent effective.

An image of Venus, made with data recorded by Japan’s Akatsuki spacecraft in 2016, shows swirling clouds in the planet’s atmosphere.
Credit: PLANET-C Project Team/JAXA

Venus is heating up—figuratively, that is. It has always been the hottest planet in the solar system, with surface temperatures of about 870 °F (465 °C). But new findings from the mysterious planet have been pouring in. Soon, a new generation of space probes will transform Venus from a sleepy solar system backwater to a bustling hub of scientific discovery.

Venus is the second planet from the sun. It is known as Earth’s “twin” because the two planets are so similar in size. The diameter of Venus is about 7,520 miles (12,100 kilometers). This diameter is about 400 miles (640 kilometers) smaller than that of Earth. No other planet comes nearer to Earth than does Venus. At its closest approach, it is about 23.7 million miles (38.2 million kilometers) away.

But Venus is better described as Earth’s evil twin, in respect to its withering conditions. In addition to the high temperatures, the atmospheric pressure is 90 times greater than that on Earth. Carbon dioxide makes up most of the atmosphere. The skies are strewn with clouds of sulfuric acid.

Scientists sent several probes to learn more about the planet in the 1960’s and 1970’s. But as space agencies learned of its inhospitable conditions, they concentrated their efforts elsewhere, particularly Mars. The last United States National Aeronautics and Space Administration (NASA) mission to study Venus, called Magellan, launched in 1990. Thus, scientists know relatively little about Venus, despite its close proximity to Earth and its similar size.

Despite the dearth of missions in recent years, planetary scientists continue to scan the planet with Earth-based instruments and reanalyze older data. They have returned surprising results.

Last year, a team of scientists announced that they had discovered a gas called phosphine in Venus’s atmosphere. Many living things on Earth produce phosphine; and scientists have not been able to identify any non-biological processes on Venus that might produce it. This raised the possibility that microbial life could exist in Venus’s atmosphere, where the conditions are much milder. But the discovery has been controversial. Other teams have failed to find any phosphine signature.

Last month, a team led by researchers at Queen’s University Belfast left the floating-Venusian-microbes idea high and dry. They found that Venus’s atmosphere does not contain enough water vapor to support life, irrespective of the presence of phosphine. The team determined that even the most extreme microbes on Earth require an environment with dozens of times more water than is available in Venus’s atmosphere.

Another recent study has shed light onto possible changing of Venus’s surface. Previously, Earth was the only rocky planet known to have a moving surface. A team lead by Paul Byrne, a professor at North Carolina State University, found evidence that parts of Venus’s surface might be slowly moving today. Earth’s crust slowly reshapes itself by a process called plate tectonics. Large pieces of the surface, called plates, subduct (sink) under one another, forming mountain ranges and other features. New crust forms along the ridges where the plates pull away from each other. In contrast, Byrne’s team found that pieces of Venus’s crust move like pack ice in polar oceans. Learning more about crust movement on Venus will help scientists understand how such processes develop on other planets, including Earth and exoplanets that might harbor life.

Last month, space agencies announced that not one, but three missions will be exploring Venus in the next 15 years. On June 2, NASA announced it is sending two mission to Venus. The missions were selected as part of part of NASA’s lower-cost Discovery Program. NASA expects to launch both missions between 2028 and 2030.

VERITAS (Venus Emissivity, Radio Science, InSAR, Topography, and Spectroscopy) will orbit the planet and map its surface with greater detail than ever before. It will allow scientists to better understand the planet’s features.

DAVINCI+ (Deep Atmosphere Venus Investigation of Noble gases, Chemistry, and Imaging) consists of a sphere that will plunge through Venus’s thick atmosphere, studying the atmosphere’s composition. The DAVINCI+ mission planners are seeking evidence of an ocean of water that might have covered Venus’s surface eons ago.

There are other players in the new Venus boom. Last year, American company Rocket Lab announced plans to launch a small probe to Venus as early as 2023. And on June 10, just over a week after NASA’s selection DAVINCI+ and VERITAS, the European Space Agency (ESA) announced that it would also be sending a probe Venus. The EnVision orbiter will search for signs of current and former tectonic activity and the presence of a past ocean. EnVision is scheduled to arrive at Venus in 2034 or 2035.

The desire to learn more about Venus is fed by more than just curiosity about our nearest neighbor. Astronomers are looking for signs of life on exoplanets. But Venus and Earth would look quite similar from light-years away. Learning more about Venus and how it evolved to become so different from Earth will help astronomers better weed out Venus-like exoplanets in their search for ones that are more like Earth.