Monday, January 22, 2024

Scientific first: Researchers find traces of disease in dolphin poop

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spinner dolphin in water

Scientists have found a new non-invasive way to identify a deadly virus in dolphins that could be a testing breakthrough. For the first time, researchers at the University of Hawaiʻi Health and Stranding Lab have successfully detected Fraser’s morbillivirus, which can cause respiratory and neurological disease, in the feces of a dolphin. The findings published in Marine Mammal Science provide a new tool to identify and monitor threats faced by Hawaiʻi’s marine mammals.

This is particularly important for Hawaiʻi’s dolphin populations, where a disease outbreak could have devastating effects. Marine mammals, recognized as sentinels of ocean health, have an important role in maintaining the delicate balance of marine ecosystems.

person in a lab
(Photo credit: U.S. Commander Pacific Fleet Environmental Readiness Division)

Researchers collected feces from a stranded dolphin infected with the virus and conducted experiments to simulate the detection of the disease in seawater. The team demonstrated the surprising ability to detect Fraser’s morbillivirus in dilutions of feces in seawater at a level of 1 to 1,000. Using this non-invasive approach, testing poop collected from live animals in the wild will enable researchers to assess the health status of marine mammals with a hands-off approach.

“This is the first time that a pathogen responsible for mass mortalities of dolphins and whales, and that affects multiple organ systems other than the digestive tract, has been demonstrated in the feces of whales and dolphins,” said Kristi West, lead author and an associate researcher at the Hawaiʻi Institute of Marine Biology.

Testing in the wild

Morbilliviruses have been responsible for mass mortalities of dolphins and whales during outbreak events. This study recommends that permitted research vessels studying dolphins and whales collect fecal samples using flasks and nets to test for disease.

“It is logistically difficult to test live, wild dolphins for the presence of disease, and the current study provides a method that can be applied to detect infectious disease in live dolphins and whales,” said Cody Clifton, a co-author and graduate student at the College of Tropical Agriculture and Human Resources.

The research was funded by the U.S. Navy and NOAA Fisheries. Reporting distressed or deceased marine mammals provides vital information for understanding causes of mortality and evaluating threats to protected species in Hawaiʻi and the greater Pacific. Sightings can be reported to the NOAA hotline at 1-888-256-9840.

Congo’s blackwater Ruki River is a major transporter of forest carbon - new study

THE CONVERSATION
Published: January 21, 2024
River Ruki. Photo by Matti Barthel, Author provided


The Congo Basin of central Africa is well known for its network of rivers that drain a variety of landscapes, from dense tropical forests to more arid and wooded savannas. Among the Congo River’s large tributaries, the Ruki is unique in its extremely dark colour, which renders the water opaque below a few centimetres’ depth.

This large blackwater river caught the attention of our carbon biogeochemistry research team when we visited its confluence with the Congo River at the city of Mbandaka. Mbandaka is a small city in the Democratic Republic of Congo, located about 600km upstream from Kinshasa on the Congo River. The area around Mbandaka is known as the Cuvette Centrale and is characterised by its vast low-lying topography, much of which floods during the rainy season and results in extensive swamp forests.

As we watched the placid dark water of the Ruki flow by, we wondered just how much carbon this river was transporting and where it came from. To answer these questions, we decided to measure the carbon in the Ruki for one year to account for seasonal changes.

The results of this study show that the Ruki is a major contributor of dissolved carbon to the Congo River, and that the majority of this carbon is sourced from the leaching of forest vegetation and soils. These results also suggest that the way in which calculations are made about how much carbon tropical forests accumulate might be off the mark – perhaps slightly overestimated.

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These findings are important because rivers are major conduits of carbon from land to ocean and atmosphere, supplying organic matter to downstream ecosystems and carbon dioxide to the air. It is important to quantify how much carbon they are moving, where it is coming from, and where it ends up. Such accounting helps scientists understand how different ecosystems function, what role they play in the carbon cycle, and how they might respond to future or ongoing human perturbations such as climate or land-use change.
The heart of the forest

The Ruki River lies at the centre of the Congo Basin. It drains a uniquely homogeneous 188,800km² of pristine lowland and swamp forests. Since climate, vegetation, soils, geology and the concentration of human impacts vary widely across Earth’s surface, it’s uncommon for a watershed of this size to have such uniform land cover. There are likely no other such uniform watersheds of this size on earth.


River Ruki. Travis Drake

This means we had an opportunity to pinpoint how a specific land cover influences the quantity and composition of organic material leached from decomposing plants and soils and carried by rainwater to river channels. Knowing this, we can “unmix” the signals measured in the Congo River and better ascertain the differences in carbon export between the many tributaries and land covers of the basin.

We found that Ruki supplies 20% of the dissolved carbon in the Congo River though it makes up only 5% of the Congo’s watershed by area. This contribution is so high because the Ruki’s water is extremely concentrated in dissolved organic matter. In fact, it is significantly richer in dissolved carbon than even the Amazon’s Rio Negro (“Black River”), which is famous for its black colour also stemming from high concentration of organics.

Water with very high concentrations of organic matter signals neither a good nor bad thing. It just means lots of carbon is contained in the water.

Because the Ruki watershed is so flat, rainwater drains slowly and has plenty of time to leach organic material from its dense vegetation. It’s like leaving multiple bags of tea to steep in water over a long period of time.

One of the reasons we wanted to know where these organic compounds were originating from is that large areas of the Ruki are underlain by enormous tracts of peat-like soils. These organic-rich soils have accumulated over hundreds to thousands of years from the buildup of partially decomposed plant matter.

If this peat was being leached or eroded into the river, through some form of disturbance, it could be released as carbon dioxide into the atmosphere and compound the greenhouse effect, much like the unearthing and combustion of fossil fuels.

Our radiocarbon isotopic measurements of the dissolved carbon indicate that there is very little peat carbon entering the river (none of it is very old), and that the dissolved carbon is sourced instead from forest vegetation and recently formed soil.

This is good news for now, but it’s something to keep an eye on if periods of drought or human activity disturb these carbon-rich peat soils.
Balancing the forest sink

Why does it matter if the Ruki transports a large amount of carbon?

One answer is that the carbon lost from terrestrial ecosystems to rivers can determine whether forests are taking up more carbon from the atmosphere (sinks) than releasing it (source) to the atmosphere. Most assessments of the balance (carbon coming in versus carbon going out of a forest) fail to account for the carbon that moves laterally to rivers.

In the case of the Ruki, the high amount of carbon that is contained in the river per unit area of the watershed suggests that this lateral movement of carbon from the Congo’s lowland forests comprises a significant proportion of the carbon balance, that is, the difference between what is coming in from photosynthesis and what is returned via respiration.

Thus, tropical forests like those around the Ruki might not accumulate quite as much carbon as we once thought. Further research is required to pin down whether this is the case. But our work on the Ruki already indicates that areas drained by such blackwater rivers may be particularly prone to carbon accounting errors like this.



Authors
Travis Drake
Postdoctoral Researcher, Swiss Federal Institute of Technology Zurich
Johan Six
Professor of Sustainable Agrosystems, Swiss Federal Institute of Technology Zurich
Matti Barthel
Research Technician, Swiss Federal Institute of Technology Zurich

Disclosure statement

Travis Drake received funding from the Swiss National Science Fund.

Johan Six received funding from Swiss National Science Fund.

Matti Barthel receives funding from Swiss National Science Fund.
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Billions of cicadas will buzz this spring as two broods emerge at the same time

JANUARY 21, 2024
Clare Marie Schneider


A cicada sheds its nymph shell in Chevy Chase, Md., during the emergence of Brood X in May 2021.
Carolyn Kaster/AP file photo

Much of the eastern United States can prepare for what one entomologist described as a "spectacular, macabre Mardi Gras" this spring.

The event Jonathan Larson, an extension entomologist at the University of Kentucky, is referring to is the simultaneous emergence of two cicada broods that will erupt in states from Virginia to Illinois come late April through June.

Periodical cicadas, which have the longest known insect life cycle, spend most of their life underground in an immature nymph form before surfacing from the ground every 13 or 17 years for a brief adult life. A brood constitutes multiple species of cicadas that merge on the same cycle.

"It's like a graduating class that has a reunion every 17 or 13 years," says Gene Kritsky, professor emeritus of biology at Mount St. Joseph University and author of A Tale of Two Broods: The 2024 Emergence of Periodical Cicada Broods XIII and XIX.


Brood X Cicadas Are Busy And So Are The Scientists Who Study Them

Although cicadas are a valuable food source for birds and small mammals, in large numbers their deafening calls can be annoying and their carcasses littering the ground can be a nuisance. The last time the Northern Illinois Brood emerged 17 years ago, "they were out in such abundant numbers that Chicagoans were having to remove them with shovels, to clear sidewalks and roads," said Floyd Shockley, an entomologist and the collections manager for the Department of Entomology at the National Museum of Natural History.

The last time the two broods — Brood XIX and Brood XIII — emerged simultaneously was in 1803. Shockley says their surfacing makes for an "extremely rare, once-in-a-lifetime event."

Brood XIX, known as the Northern Illinois Brood, contains three different species of cicadas and emerges only every 17 years. The Great Southern Brood, or Brood XIII, is on a 13-year cycle and contains four different species of cicadas.

Shockley says the Great Southern Brood will start appearing in late April through the first or second week of May across 15 states, mostly in the South, running from Virginia and into Alabama and Mississippi.


No, You Don't Need To Be Worried Your Dog (Or Cat) Is Eating Cicadas

As for the Northern Illinois Brood, Shockley says people will start to see these cicadas closer to mid-May through the first week of June. The brood will be highly concentrated across four states, including Illinois, parts of Wisconsin, Indiana, and a bit of Michigan.

Across the east, Kritsky says, "we'll probably see billions of cicadas" due to the dual emergence of the two broods. While you may hear or see cicadas in your area well into September, the perennial cicadas will die off by June, their song replaced by annually occurring cicadas for the rest of the summer.

Once the ground reaches the optimal temperature of 64 degrees Fahrenheit, the insects find their way to nearby trees and shed their skins, Kritsky said. It takes about four to five days for the adult males to start singing, but once they do, their songs can be louder than a jet engine.

The male cicadas "produce this chorus that attracts the females to the trees," says Larson. "Then they'll pair up and have courtship songs," singing individually to female cicadas in an attempt to persuade them to mate. After mating, the female cicada lays her eggs in a tree and then they die, littering the base of trees and leaving behind what Kritsky describes as a "delicate, rotten Limburger cheese" smell.

The cycle begins all over when the cicada eggs drop from the tree, returning to the ground for another 13 to 17 years. Although they spend years underground in an immature state, the adult lifespan of a cicada ranges only from four to six weeks.


Here Come The Cicadas

"It's pretty much this big spectacular macabre Mardi Gras," says Larson. "It's a lot of singing, lots of paramours pairing up, and then lots of dying."

While the two broods this spring will mostly be separated by time and place, "they will overlap for several weeks," in Illinois, says Shockley. This overlap could result in some Illinois residents hearing all seven species of the two broods singing their cacophonous mating calls together, he says. Additionally, Shockley says the overlap could result in "an extremely rare opportunity for genetic crossing between 13-year cicadas and 17-year cicadas that could lead to the emergence of a new brood."

All the experts NPR spoke with emphasized that the bugs' ephemeral emergence is not harmful to humans or pets. While the sheer amount of them may be shocking if you're in certain high density areas, they won't bite or sting you, says Larson. "Your pets will probably try to eat them," he adds. "And they're going to be OK."

Shockley added not to spray pesticides on the bugs. The chemicals could impact birds and small mammals that might feed on the cicadas. "Or it could hit non-target things like butterflies and bees that you actually want to have around your home," he says.

While Larson says people may be "disgusted by the situation," he emphasized that it's a unique, beautiful spectacle of nature that you can't encounter elsewhere in the world.

Kritsky described the short-lived emergence of the cicadas as "like having a David Attenborough special in your backyard," referring to the British naturalist and broadcaster. "If you're lucky enough to live in an area where these things are going on, get your kids out there. Watch this."

Research suggests European Alps eroding slower than >10,000 years ago



Rothorn Glacier in Hungerli Valley, Switzerland, is a bowl-shaped depression cirque glacier and the study site of rockwall erosion. Key glacial landforms are also identified; talus slopes form due to debris from rockfall events, while moraine ridges are unconsolidated debris deposited at the snout of a glacier and can be clear indicators of its retreat through time. LIA refers to the extent of the glacier during the Little Ice Age (1250 - 1860 AD). Credit: Draebing et al. 2024.

Deglaciation during the Holocene (last ~17,000 years) has had significant impacts on the surrounding mountainous environments as glaciers retreated and left distinct landforms in their wake, such as debris ridges (moraines) deposited at the snout during retreat.

Further adding to this is the rate of erosion of the 'newly' exposed , which cause rockfall events, and is the focus of new research published in Earth and Planetary Science Letters which suggests  may be declining in more recent decades/centuries compared to earlier in the Holocene.

Dr. Daniel Draebing, of Utrecht University, Netherlands, and colleagues have studied the slopes of mountain bedrock (termed rockwalls) of the European Alps to test the role of climate warming in this change of erosion rates. The theory pertains to reduced glacial load since the last peak glacial period of the Younger Dryas (~12,900–11,700 years ago), causing a reduction in glacial debuttressing and therefore a decline in exposure of steep valley sides to erosion.

Combining real-world field data with modeling, the research team calculated 1.2–1.4 mm/year erosion rates for a periglacial alpine valley in southern Switzerland at ~9,000–10,000 years ago, based on debris at the base of the rockwall (talus slopes), and compared them to modern measurements of 0.02–0.08 mm/year erosion rates between 2016 and 2019.

Specifically, the scientists reconstructed the glacial retreat history of the Hungerli Valley, focusing on the temperature of the rockwalls and how this may have affected the occurrence of permafrost (rock/soil material that remains below 0°C throughout the year) and frost cracking (splitting of bedrock caused by freezing water).

The latter forms due to a process known as ice segregation, Dr. Draebing explains, adding, "Water freezes to ice and the ice draws additional water to the ice body, causing it to increase in size and produce stress that breaks down the rock."

Modeling frost cracking through time is based upon the percentage change in the porosity of the metamorphosed paragneiss and schist slate bedrock through fractures, fed by laboratory data testing the strength of samples taken from the study site.

Both permafrost and frost cracking weaken the rockwalls, leading to rockfall events, which may be further exacerbated by seismic activity occurring from changes in land stresses with the 'weight' of a glacier (glacial loading) being removed during melting.

Laser scanning surveys helped the research team to record changes in rockfall activity in the Hungerli Valley over the modern study period, identifying 263 events, with a maximum volume of 159.4 m3 for a single event. Such events were a hazard to the scientists during their , with Dr. Draebing saying, "Working in high-alpine environments is very demanding for a team physically and psychologically, and active rockfall is dangerous so these hazards had to be evaluated every day."


A) Rothorn Glacier retreat history with numbered rockwalls investigated in this study. B) Reconstructed mean annual rock surface temperature (MARST) and size of rockfall events detected from laser scanning in the Hungerli Valley, Switzerland. Credit: Draebing et al. 2024.

Dr. Draebing and colleagues found that higher average rates of erosion occurred throughout the middle to late Holocene on slopes that had been free of glacial ice since ~10,000 years ago, compared to the modern day, and attribute this to elevated intensity of permafrost and frost cracking.

This effect was intensified further with elevation, as mountain rockwalls above 2700 m experienced greater erosion than lower-elevation locations during the Younger Dryas, with a peak in frost cracking in the models. However, this pattern was found to break down over time, with a  in erosion rate. For example, over the past five decades, the highest recorded erosion rate at the site of 50.7 mm/year was two orders of magnitude higher than earlier in the Holocene, but declined to just 0.58 mm/year by 2019.

An initial high but subsequent rapid decay in erosion rate is postulated to be caused by a combination of increased frost cracking, thawing of permafrost and the adjustment of the landscape to the unloading of glacial ice.

Dr. Draebing suggests it is not possible to discern which of these three factors is most dominant in erosion. "All of these processes are affected by low temperature and precipitation (especially glaciers) so it is not surprising that they occur at the same elevation range as mountain temperature is a function of elevation."

"We moved down in elevation and did a comparable study on rockwall areas that are permafrost-free and not affected by recent glaciation to identify the role of frost cracking in erosion and to work on a system where we can exclude permafrost and glacier retreat, both of which made analysis more challenging."

Seasonal snow cover also plays a part, with thicker snow layers insulating the rockwall and delaying freeze-thaw processes. Overall, the research team concludes that frequent small-scale rockfalls occur in preference to larger-scale single devastating events as a result of glacial retreat.

Concerning whether erosion rates will continue declining until a future glaciation, Dr. Draebing says, "Erosion depends upon topographic stresses (such as slope steepness) and climate-induced stresses (like frost cracking, permafrost thaw and glacier retreat). Climate-induced stresses will decrease due to climate warming, however, topographic stresses will persist. Erosion rate will reach an equilibrium probably similar to current erosion rates of 0.02 and 0.08 mm/year."

This research is important in understanding the role deglaciation in a warmer world impacts processes affecting rock erosion, and therefore rockfall events, as climate change continues. In addition to permafrost and frost cracking, extreme weather events may also enhance erosion, as well as large-magnitude earthquakes.

The impact such situations may have on the local landscape and its inhabitants is vital to support the infrastructure mountain-dwelling communities and alpine tourism resorts rely upon, as well as wildlife struggling to adapt to the changing environment.

Dr. Draebing concludes, "Due to climate change, glaciers and permafrost will disappear and frost cracking will decrease, which in the long term will result in decreasing erosion rates. However, in the short term, glacier retreat and permafrost thaw will increase  rates and rockfall hazard, something mountain communities will need to adapt themselves to in the near future."

More information: Daniel Draebing et al, Holocene warming of alpine rockwalls decreased rockwall erosion rates, Earth and Planetary Science Letters (2023). DOI: 10.1016/j.epsl.2023.118496


 

Can giant air cleaners solve the air pollution crisis?

China has constructed the world’s largest experimental air-purifying tower


In 2016, researchers in Xi’an, China — a city long plagued by air pollution — constructed the world’s largest experimental air-purifying tower. The researchers, from the Institute of Earth Environment at the Chinese Academy of Sciences, found that the surrounding area of over three square miles has improved in air quality.

Data collected in the vicinity of the experimental tower shows that this kind of tower presents promising solutions for cities contending with the escalating air pollution crisis. If similar initiatives were implemented globally, their impact could extend beyond individual cities, resulting in significant benefits for public health.

Air quality: The current landscape

Awareness of air pollution’s detrimental effects dates back several decades, when the US government was one of the first countries to introduce legislation to reduce air pollution: the Air Pollution Control Act, signed in 1955, provided funding for air pollution research. The enactment of the 1970 US Clean Air Act allowed regulators to limit emissions from both industrial sources and transportation, leading to efforts to reduce air pollution emissions, such as investments in the development of cleaner, less carbon-intensive technologies.

Despite increased awareness of air pollution, data reveals that hardly any place on Earth is spared from unhealthy air conditions. A study published in The Lancet Planetary Health journal found that only approximately 0.2 per cent of global land has been exposed to fine particulate matter — any particles that are 2.5 microns or smaller in diameter, also known as PM2.5 — at concentrations lower than the World Health Organization’s (WHO) recommended annual limit of five micrograms per cubic metre. 

This means that more than 99 per cent of global land is exposed to dangerous concentrations of fine particulate matter, which originates as a byproduct of industrial combustion and poses a significant threat to human health due to its ability to be inhaled deep into the lungs. 

A 2022 WHO report looked at findings from over 6,000 cities across 117 countries that are monitoring air quality. About 99 per cent of the global population breathes air that’s over WHO’s quality limits, with the most significant impacts on low and middle-income countries. 

WHO’s data from 2019 showed that regions with high industrial activity, like areas in southern and eastern Asia, face a heightened risk of air quality issues. In some of these places, air quality is over WHO’s daily limit — 15 micrograms of gaseous pollutants per cubic metre — for over 90 per cent of the year. This leaves the majority of the global population vulnerable to the health risks associated with chronic exposure to air pollution, such as lung cancer and heart diseases, resulting in 6.7 million premature deaths worldwide.

How does the giant air filter work? 

Standing at over 100 metres tall — and costing the Shaanxi provincial government roughly 2.69 million CAD to build — Xi’an’s air-purifying tower produces clean air at a rate of about eight cubic metres per second. The tower operates using solar energy that traps solar heat in the tower, which heats up polluted air drawn in through the tower’s base in an effect similar to the greenhouse effect. This heated air then rises through the filters within the tower.

Since its activation, the tower has cleansed more than 10 million cubic metres of air daily, significantly enhancing the air quality in its vicinity. Plans are underway to construct more towers across China in areas with unhealthy air quality levels, including Guangzhou, Hebei, and Henan. 

To assess the impact of these experimental air purifiers, Xi’an placed over a dozen pollution monitoring stations across a 10-square-kilometre area around the tower. In just a few months, preliminary results found a 15 per cent reduction in PM2.5 levels during episodes of heavy pollution.

With promising preliminary results and expansion plans to introduce these projects to more Chinese cities, other countries are taking note. Kurin Systems, an air purification company based in India, was inspired by the giant air purifier tower in Xi’an and intends to install a 12-metre purification tower in New Delhi, long plagued with poor air as one of the world’s most polluted cities, with hopes to purify 1,130 cubic metres of air per day within an area of about five square kilometres. 

Limitations and concerns for giant air purifiers

While large air filter towers hold potential for providing clean air to surrounding communities, their capacity remains local. Cao Junji, a chemist at the Chinese Academy of Sciences’ Key Laboratory of Aerosol Chemistry and Physics in Xi’an, proposed building up to half a dozen purifying towers around the city to significantly reduce air pollution. Furthermore, these air purifiers cannot replace indoor air filtration systems for buildings in highly polluted areas, such as factories and airports. In such cases, air purifiers and air filters remain the best solution for safe indoor air quality.

Critics argue that without more data regarding the power consumption for these filtration towers, the energy input required for operating these giant air purifiers seems like they might not be the best use of energy. Redirecting the same amount of power to generate clean electricity or reducing pollution at the source could also significantly reduce pollution. Other scientists worry that these towers may not effectively filter toxins that can be precursors to harmful particulate matter or liquids capable of penetrating the lungs and causing health problems, such as sulphur dioxide gas or secondary gaseous pollutants like ozone.

Nevertheless, giant air cleaners offer hope in areas where air quality is a major concern. While they may have limits and cannot single-handedly purify the air for entire cities, they serve as a valuable resource for improving air quality in regions of dangerous air quality levels where the reduction of air pollution is very difficult. They can potentially provide a temporary solution as scientists and policymakers work on strategies to reduce air pollution at its source.

Chaos is everywhere

What chaos means in science and where you can find it


Scientists have long desired to unlock the secret of chaos and order the disordered. From mathematics and philosophy to biology and psychology, many disciplines study the phenomenon of chaos.

In early science, theories of determinism proposed that events in the universe are predetermined and inevitable. Causality allows predictability, but while this idea has led to the development of countless statistical models of the universe and nature, they haven’t been able to predict everything. Random phenomena exist. Tiny changes to the initial conditions of a system can lead to enormous changes in the final product, and a small error can precede a massive one — a phenomenon whose study is known as chaos theory. 

Chaos theory is everywhere

Chaos theory explores the concept that everything in the universe tends towards chaos. In mathematics, data often has outliers — values that are extremely different from the rest of a set of data — that result from true variation within something being studied, or from error. If the variation is the result of error, then it is considered ‘noise,’ which can induce chaos in nonlinear systems — systems that don’t change linearly in proportion to their variables. 

From a philosophical perspective, chaos theory says that a fully predictable universe is impossible because the universe’s tendency to change at random prevents every process from being repeated in the exact same way every time. Physics defines chaos in a behavioural manner. Some planets’ orbits, for example, never repeat themselves — they’re irregular and therefore chaotic. Thus, we cannot fully predict planetary positions as they move along these orbits. 

In evolution, constant changes in the environment and complex interactions between competing traits have led to chaos in the evolution of phenotypes — meaning the observable traits of an organism. So, it is impossible to understand all the forces at play during the course of evolution because of chaos. Even genomes — the entire collection of DNA in a cell — are a record of randomness, since mutations — changes to a DNA sequence — and genetic drift — the change in frequency of a specific gene variant in a population due to random chance — are beyond our ability to predict and control. Yet, mutations and genetic drift are inducers of the diversity and individuality of organisms. 

With chemistry, consider the phase transition of water: boiling water is a chaotic process because its state is more unstable, whereas order is achieved in water’s solid form to maintain the structure of ice. In this way, chaos seems to increase as energy is added to a substance. 

As you contemplate chaos, consider this development: the human heart, a predictable component of our bodies, grows stronger when its rhythm faces minor deviations. In the midst of chaos, in what we can’t control, we live, and we grow.

 

Insulin: Toronto’s gift to the world

A brief explanation of how insulin improves the lives of people with diabetes


On January 23, 1922, a 14-year-old boy who was severely ill at the Toronto General Hospital became the first person to receive a purified insulin shot. That boy was Leonard Thompson, and like many others, he suffered from diabetes. 

According to the World Health Organization (WHO), about 422 million people in the world lived with diabetes in 2014. The number didn’t decline as the decade went by: more recent data from the International Diabetes Federation show about 537 million people with diabetes as of 2021. 

Although these statistics are disconcerting, it is perhaps of consolation to remember that while diabetes was once considered a fatal disease, now, with the discovery and distribution of insulin, people with diabetes can lead normal lives. It is not an overstatement to say that insulin, Frederick Banting and Charles Best’s discovery at the University of Toronto, has saved millions.

What is diabetes?

Simply put, diabetes is a chronic disease where glucose, the body’s and brain’s main fuel, cannot get into the body’s cells. Glucose comes from the food we eat or is produced by our bodies and enters the bloodstream during the digestive process. Once there, the pancreas detects the rising glucose levels in the bloodstream and releases a hormone called insulin. Insulin works like a key, opening a unique door in cell membranes so glucose can leave the bloodstream and access the cells. 

The effect is simple: glucose levels in the bloodstream decrease, and your cells will have fuel to work so your body can perform its duties, such as thinking, breathing, and moving every single muscle of your body. Yes, that includes every beat of your heart.

Now, if the insulin hormone, which plays a pivotal role in the process of glucose cellular uptake, fails to do its job, there are consequences. Depending on the reason for insulin failing to fulfill its role, people contract different types of diabetes. 

“It’s not me. It’s the pancreas”: this is the case in type 1 diabetes. Here, the pancreas — the sole organ responsible for producing and releasing insulin — produces little to no insulin, meaning that patients within this group depend on external insulin to live. This is the type that Leonard had, and it tends to appear in childhood and teenage years. Type 1 diabetes primarily stems from an auto-immune response — whose exact nature remains unknown — that affects the pancreas function. 

“It is still not me. It’s the pancreas and the cells”: this is the case of type 2 diabetes. Here, either the pancreas produces little to no insulin, or cells don’t respond to the insulin, which is also called insulin resistance. In the latter scenario, the body’s cells don’t recognize insulin as a key, and therefore, glucose won’t be able to cross the cells’ membrane. This results in overwork from the pancreas as it tries to lower rising glucose levels, a vicious cycle that can lead to the organ’s own failure. This type is mainly seen in adults because it is triggered by life factors such as diet, lack of physical activity, age, and metabolic conditions. 

There are other types of diabetes which are mostly associated with very specific conditions. For example, gestational diabetes occurs during pregnancy in women who weren’t diagnosed with diabetes before. If treated correctly, the condition will reverse after childbirth; if not, there may be severe and life-threatening consequences for the fetus. 

What happens if insulin doesn’t do its job? 

Our body cells interact with specific molecules via “mediators.” Insulin is one of these mediators. It arrives at the cell membrane and triggers a cascade of events that transports the glucose through the membrane, as cells won’t interact directly with glucose due to the glucose’s size and molecular complexity. So, if the insulin doesn’t help the glucose get into the cell, glucose will keep flowing in the bloodstream. 

A high glucose level in the blood is called hyperglycemia, and it can become dangerous for various reasons. Firstly, glucose is sticky. Similar to when you overload your coffee with sugar so that the drink becomes thicker, glucose will make blood more viscous and sticky. The more glucose is present in the blood, the more likely the big molecule will adhere to the membranes of the tissues it encounters while travelling through the bloodstream. 

In particular, glucose will eventually adhere in the eyes, causing blindness; the kidneys, ending in renal failure; the heart, causing strokes and heart attacks; the vascular system, causing clogged veins and atherosclerosis; and the nerves, leading to a loss of mobility, especially in feet and legs. Combined with damage to the vascular system, diabetes-caused damage to the nerves can end in amputations. The overall consequence of untreated diabetes is a progressive organ failure that is not compatible with life. 

Secondly, and most importantly, hyperglycemia’s persistence over time can lead to what an untreated diabetic patient will experience as symptoms of diabetes. Although not all individuals are the same and, therefore, experience different things, initially, it is most likely that hyperglycemia will increase the rate at which a person urinates; tons of glucose in the blood require the kidneys to work harder to filter it out of the blood via urine. The more you urinate, the more water you need to drink, so uncontrollable thirst is another symptom of diabetes. 

In addition, someone with hyperglycemia might feel extreme tiredness and experience weight loss. Although there is tons of glucose in the bloodstream, insulin is not there to help it get inside the cells. When the cells are not receiving fuel, they will send signals to the brain for you to eat, eat, and eat. 

Under this panorama, a person with these symptoms might feel irritated and have intense headaches, including blurred vision. If the hyperglycemic state remains uncontrolled over time, it will lead to organ damage and progressive organ dysfunction. 

The gift of insulin, the medicine

Today, over a hundred years after that early morning when Banting woke up to draft a 25-word hypothesis to cure diabetes on a piece of paper, insulin is one of the best medicines we can use to control hyperglycemia. 

The administration of external insulin into the body is a resource used by millions of people with diabetes every day. Nowadays, multiple devices are available that help people with diabetes sense their glucose levels and better dose an insulin shot. 

Insulin, as medicine, is vital for patients with type 1 diabetes, where their pancreas produces insufficient insulin. This contrasts with type 2 patients, where adequate care and diet can leave an insulin shot as a last resort. In fact, an early diagnosis of type 2, in a stage called pre-diabetes, an accurate treatment design from physicians and dietitians that patients adhere to can result in the ability to avoid insulin therapy altogether. 

The science and technology applied to research over the years since insulin’s discovery have helped to make better diagnoses and treatments. Challenges for people with diabetes today include accessibility to insulin as a medicine, a need for better delivery methods for the drug administration to improve life quality, and lastly, an overall social change regarding diet, physical activity, stress management and work/life balance. 

The effect of Banting and Best’s discovery at U of T is powerful. Imagine Leonard Thompson coming in and out of unconsciousness and receiving the first purified insulin shot, showing signs of improved health and subsequently going on to live. This was a miraculous outcome. 

A U of T surgeon described patients with diabetes after taking insulin as being “awakened dramatically, snatched from death’s door.” This is all thanks to the endeavours of Banting, Best, J. J. R. Macleod — an international expert in diabetes who pushed Banting to pursue his idea — and James B. Collip, who helped purify the extract, making it safe for human trials. What a riveting story of collaboration and creativity, based here, at U of T.


GEMOLOGY
A major explosion could see "fountains of diamonds" erupt from the Earth's crust during a geological event.

When rock combines with water, carbon dioxide and diamonds they can create an explosive rush (
Image: Getty Images)

ByGraeme Murray
News Reporter21 Jan 2024

A major explosion could see "fountains of diamonds" erupt from the Earth's crust during a geological event.

Research by Thomas Gernon, a professor of Earth and climate science at the University of Southampton, suggests supercontinents could split and send diamonds flying form the centre of the Earth. The precious stones form 150 kilometres below our feet, but the professor predicts they will be sent skywards by 'kimberlite' eruptions at 133 kilometres an hour sparking enormous explosions on the planet's surface according the the study which is published in the journal Nature.

Gernon and his researchers analysed kimberlites - rock which contains diamonds - and found eruptions regularly happen millions of years later when plates start to pull apart. An example happened around 25 million years after the supercontinent Gondwana started breaking up into what is now Africa and South America.

The pulling apart of the plates leads to rock from the upper mantle and lower crust to mix and flow against each other, causing instability and ultimately leading to the eruptions. This also sees rock, water and carbon dioxide combining with minerals like diamonds. And when they mix they create explosive rushes towards the surface of the Earth. The research team hope their work could help find unexplored diamond deposits.

Gernon said: "The diamonds have been sat at the base of the continents for hundreds of millions or even billions of years. There must be some stimulus that just drives them suddenly, because these eruptions themselves are really powerful, really explosive."

Kimberlites happen when high-pressure eruptions o break through rock as they ascend to the earth's surface 
Image: 
Alamy Stock Photo)
Samples of laboratory-grown type rough diamonds 
Image: 
Bloomberg via Getty Images)

The Mirror reported in 2019 how scientists discovered a tiny speck of rock inside a diamond s made from a mineral never before seen on Earth. It is thought to have formed at a depth of about 105 miles below the surface and was retrieved from South Africa's Koffiefontein diamond mine. The opaque, dark green speck of rock inside has an unusual chemical signature, sparking questions about the composition of Earth's mantle. It was named goldschmidtite in honour of the founder of modern geochemistry Victor Moritz Goldschmidt.

Researchers said it offered a unique record of chemistry from a long time ago, inside the deep, ancient parts of the planet. Nicole Meyer, a PHD student from the University of Alberta discovered the mineral. She said: "Goldschmidtite has high concentrations of niobium, potassium, and the rare earth elements lanthanum and cerium, whereas the rest of the mantle is dominated by other elements, such as magnesium and iron.”

She added: "For potassium and niobium to constitute a major proportion of this mineral, it must have formed under exceptional processes that concentrated these unusual elements." The mantle is the thick layer of hot, solid rock between the Earth's crust and its molten iron core. It starts about 20 miles below the surface and is about 1800 miles thick.