The University of Cambridge study used data from more than 10,000 people born between 2000 and 2002 to understand the long-term interplay between our early relationships with our parents, prosociality and mental health. It is one of the first studies to look at how these characteristics interact over a long period spanning childhood and adolescence.

The researchers found that people who experienced warm and loving relationships with their parents at age three not only tended to have fewer mental health problems during early childhood and adolescence, but also displayed heightened ‘prosocial’ tendencies. This refers to socially-desirable behaviours intended to benefit others, such as kindness, empathy, helpfulness, generosity and volunteering.

Although the correlation between parent-child relationships and later prosociality needs to be verified through further research, the study points to a sizeable association. On average, it found that for every standard unit above ‘normal’ levels that a child’s closeness with their parents was higher at age three, their prosociality increased by 0.24 of a standard unit by adolescence.

Conversely, children whose early parental relationships were emotionally strained or abusive were less likely to develop prosocial habits over time. The researchers suggest this strengthens the case for developing targeted policies and support for young families within which establishing close parent-child relationships may not always be straightforward; for example, if parents are struggling with financial and work pressures and do not have much time.

The study also explored how far mental health and prosocial behaviour are fixed ‘traits’ in young people, and how far they fluctuate according to circumstances like changes at school or in personal relationships. It measured both mental health and prosociality at ages five, seven, 11, 14 and 17 in order to develop a comprehensive picture of the dynamics shaping these characteristics and how they interact.

The research was undertaken by Ioannis Katsantonis and Dr Ros McLellan, both from the Faculty of Education, University of Cambridge.

Katsantonis, the lead author and a doctoral researcher specialising in psychology and education, said: “Our analysis showed that after a certain age, we tend to be mentally well, or mentally unwell, and have a reasonably fixed level of resilience. Prosociality varies more and for longer, depending on our environment. A big influence appears to be our early relationship with our parents. As children, we internalise those aspects of our relationships with parents that are characterised by emotion, care and warmth. This affects our future disposition to be kind and helpful towards others.”

The study used data from 10,700 participants in the Millennium Cohort Study, which has monitored the development of a large group of people born in the UK between 2000 and 2002. It includes survey-based information about their prosociality, ‘internalising’ mental health symptoms (such as depression and anxiety) and ‘externalising’ symptoms (such as aggression).

Further survey data provided information about how far the participants’ relationships with their parents at age three were characterised by ‘maltreatment’ (physical and verbal abuse); emotional conflict; and ‘closeness’ (warmth, security and care). Other potentially confounding factors, like ethnic background and socio-economic status, were also taken into account.

The Cambridge team then used a complex form of statistical analysis called latent state-trait-occasion modelling to understand how far the participants’ mental health symptoms and prosocial inclinations seemed to be expressing fixed personality ‘traits’ at each stage of their development. This enabled them, for example, to determine how far a child who behaved anxiously when surveyed was responding to a particular experience or set of circumstances, and how far they were just a naturally anxious child.

The study found some evidence of a link between mental health problems and prosociality. Notably, children who displayed higher than average externalising mental health symptoms at a younger age showed less prosociality than usual later. For example, for each standard unit increase above normal that a child displayed externalising mental health problems at age seven, their prosociality typically fell by 0.11 of a unit at age 11.

There was no clear evidence that the reverse applied, however. While children with greater than average prosociality generally had better mental health at any single given point in time, this did not mean their mental health improved as they got older. On the basis of this finding, the study suggests that schools’ efforts to foster prosocial behaviours may be more impactful if they are integrated into the curriculum in a sustained way, rather than being implemented in the form of one-off interventions, like anti-bullying weeks.

As well as being more prosocial, children who had closer relationships with their parents at age three also tended to have fewer symptoms of poor mental health in later childhood and adolescence.

Katsantonis said that the findings underlined the importance of cultivating strong early relationships between parents and children, which is already widely seen as critical to supporting children’s healthy development in other areas.

“So much of this comes back to parents,” Katsantonis said. “How much they can spend time with their children and respond to their needs and emotions early in life matters enormously.”

“Some may need help learning how to do that, but we should not underestimate the importance of simply giving them time. Closeness only develops with time, and for parents who are living or working in stressful and constrained circumstances, there often isn’t enough. Policies which address that, at any level, will have many benefits, including enhancing children’s mental resilience and their capacity to act positively towards others later in life.”

The radiocarbon spike was caused by a massive solar storm, the biggest ever identified. 

A similar solar storm today would be catastrophic for modern technological society — potentially wiping out telecommunications and satellite systems, causing massive electricity grid blackouts, and costing us billions of pounds. 

The academics are warning of the importance of understanding such storms to protect our global communications and energy infrastructure for the future.         

The collaborative research, which was carried out by an international team of scientists, is published today (Oct 9) in The Royal Society’s Philosophical Transactions A: Mathematical, Physical and Engineering Sciences and reveals new insights into the Sun’s extreme behaviour and the risks it poses to Earth.  

A team of researchers from the Collège de France, CEREGE, IMBE, Aix-Marseille University and the University of Leeds measured radiocarbon levels in ancient trees preserved within the eroded banks of the Drouzet River, near Gap, in the Southern French Alps.   

The tree trunks, which are subfossils — remains whose fossilization process is not complete — were sliced into tiny single tree-rings. Analysis of these individual rings identified an unprecedented spike in radiocarbon levels occurring precisely 14,300 years ago. By comparing this radiocarbon spike with measurements of beryllium, a chemical element found in Greenland ice cores, the team proposes that the spike was caused by a massive solar storm that would have ejected huge volumes of energetic particles into Earth’s atmosphere. 

Edouard Bard, Professor of Climate and Ocean Evolution at the Collège de France and CEREGE, and lead author of the study, said: “Radiocarbon is constantly being produced in the upper atmosphere through a chain of reactions initiated by cosmic rays. Recently, scientists have found that extreme solar events including solar flares and coronal mass ejections can also create short-term bursts of energetic particles which are preserved as huge spikes in radiocarbon production occurring over the course of just a single year.” 

Potentially catastrophic

The researchers say that the occurrence of similar massive solar storms today could be catastrophic for modern technological society, potentially wiping out telecommunications, satellite systems and electricity grids - and costing us billions of pounds. They warn that it is critical to understand the future risks of events like this, to enable us to prepare, build resilience into our communications and energy systems and shield them from potential damage. 

Tim Heaton, Professor of Applied Statistics in the School of Mathematics at the University of Leeds, said: “Extreme solar storms could have huge impacts on Earth. Such super storms could permanently damage the transformers in our electricity grids, resulting in huge and widespread blackouts lasting months. They could also result in permanent damage to the satellites that we all rely on for navigation and telecommunication, leaving them unusable. They would also create severe radiation risks to astronauts.”    

Miyake Events

Nine such extreme solar storms — known as Miyake Events — have now been identified as having occurred over the last 15,000 years. The most recent confirmed Miyake Events occurred in 993 AD and 774 AD. This newly-identified 14,300-year-old storm is, however, the largest that has ever been found — roughly twice the size of these two. 

The exact nature of these Miyake Events remains very poorly understood as they have never been directly observed instrumentally. They highlight that we still have much to learn about the behaviour of the Sun and the dangers it poses to society on Earth. We do not know what causes such extreme solar storms to occur, how frequently they might occur, or if we can somehow predict them.  

Professor Bard said: “Direct instrumental measurements of solar activity only began in the 17th century with the counting of sunspots. Nowadays, we also obtain detailed records using ground-based observatories, space probes, and satellites. However, all these short-term instrumental records are insufficient for a complete understanding of the Sun. Radiocarbon measured in tree-rings, used alongside beryllium in polar ice cores, provide the best way to understand the Sun’s behaviour further back into the past.” 

The largest, directly-observed, solar storm occurred in 1859 and is known as the Carrington Event. It caused massive disruption on Earth — destroying telegraph machines and creating a night-time aurora so bright that birds began to sing, believing the Sun had begun to rise. However, the Miyake Events (including the newly discovered 14,300-yr-old storm) would have been a staggering entire order-of-magnitude greater in size. 

Professor Heaton said: “Radiocarbon provides a phenomenal way of studying Earth’s history and reconstructing critical events that it has experienced. A precise understanding of our past is essential if we want to accurately predict our future and mitigate potential risks. We still have much to learn. Each new discovery not only helps answer existing key questions but can also generate new ones.” 

Cécile Miramont, Associate Professor of Paleoenvironments and Paleoclimates at IMBE, Aix-en-Provence University, said: “Finding such a collection of preserved trees was truly exceptional. By comparing the widths of the individual tree rings in the multiple tree trunks, we then carefully pieced together the separate trees to create a longer timeline using a method called dendrochronology. This allowed us to discover invaluable information on past environmental changes and measure radiocarbon over an uncharted period of solar activity.” 

Understanding the movements of the tectonic plates that make up the earth’s rigid outer shell is essential to understand the planet’s geological history. The movements of these plates strongly influenced how the planet’s paleogeography and climate have changed over time, and even where to find rare metals. But large oceanic plates from the geological past have since disappeared into the earth’s mantle by means of subduction. They have left behind only fragments of rock hidden in mountain belts. Van de Lagemaat studied the planet’s most complicated plate tectonic region: the area around the Philippines. “The Philippines is located at a complex junction of different plate systems. The region almost entirely consists of oceanic crust, but some pieces are raised above sea level, and show rocks of very different ages.”

Reconstruction

Using geological data, Van de Lagemaat first reconstructed the movements of the current plates in the region between Japan and New Zealand. That revealed how large the area was of plates that must have disappeared in the current western Pacific region. “We also conducted field work on northern Borneo, where we found the most important piece of the puzzle. We thought we were dealing with relicts of a lost plate that we already knew about. But our magnetic lab research on those rocks indicated that our finds were originally from much farther north, and had to be remnants of a different, previously unknown plate.” But the important realisation was yet to come. “11 years ago, we thought that the remnants of Pontus might lie in northern Japan, but we’d since refuted that theory,” explains Douwe van Hinsbergen, Van de Lagemaat’s PhD supervisor. “It was only after Suzanna had systematically reconstructed half of the ‘Ring of Fire’ mountain belts from Japan, through New Guinea, to New Zealand that the proposed Pontus plate revealed itself, and it included the rocks we studied on Borneo.”

Relics

The relics of Pontus are not only located on northern Borneo, but also on Palawan, an island in the Western Philippines, and in the South China Sea. Van de Lagemaat’s research also showed that a single coherent plate tectonic system stretched from southern Japan to New Zealand, and it must have existed for at least 150 million years. That is also a new discovery in the field.

Waves

The previous predictions of the existence of Pontus were made possible because a subducted plate leaves behind traces when it ‘sinks’ into the earth’s mantle: zones in the mantle with anomalous temperatures or compositions. These anomalies can be observed when seismographs pick up signals from earthquakes. Earthquakes send waves through Earth’s interior, and when they travel through an anomaly, such as a fragment from an old plate, the anomaly produces a disruption of the signal. Geologists can trace these disruptions to the existence of phenomena in the mantle, such as fragments of tectonic plates. That allows them to look 300 million years into the past; older plate fragments have ‘dissolved’ at the boundary between the mantle and the core. The study from 11 years ago showed that a large subduction zone must have run through the western paleo-Pacific Ocean, which separated the known Pacific plates in the east from the hypothetical Pontus plate in the west. This hypothesis has now been independently demonstrated by Van de Lagemaat’s research.

“Freshwater habitats in general are getting saltier for a number of reasons, including road salt and agricultural runoff, extraction of coal and natural gas, drought, and sea level rise,” says David Buchwalter, professor of toxicology at NC State and corresponding author of the research. “Freshwater insects and other organisms that live in these systems are used as indicators of the ecosystem’s health. When these systems get saltier, we see that insect diversity decreases, but we aren’t sure why.”

Aquatic animals (including insects and crustaceans) must constantly maintain the correct balance of water and salts within their body — a process called osmoregulation. Theoretically, the most favorable environment for aquatic animals would be one where external salinity levels are close to those inside the animal. That way the animal doesn’t have to work as hard to maintain osmoregulation.

However, the opposite seems to be true for freshwater insects — higher salinity is always associated with increased rates of ion uptake in insects, but it is also associated with developmental delays or death.

“We thought that freshwater insects might be shifting so much of their energy toward osmoregulation in saltier environments that they cannot grow or thrive,” Buchwalter says. “So we measured the metabolic rates of crustaceans and insects in dilute and saline environments to see if metabolic responses to salinity were similar.”

The team looked at three types of freshwater animals — two species of gammarid, or “scud,” which is a small freshwater crustacean; one freshwater snail; and three aquatic insect species.

In the first test, they measured the animals’ metabolism by placing them in waters with different concentrations of salt ions and looking at their rates of oxygen consumption. They observed that more dilute conditions made the crustaceans and snail breathe harder, increasing their metabolism, while insects’ metabolic rates were constant regardless of salinity.

Next, the team looked at whether an increase in breathing rates was linked to the transport of a particular ion. Radioactive isotopes of the salt ions calcium and sodium allowed the researchers to measure how much and how quickly the animals took up different ions.

The researchers found that calcium was the key driver of non-insects’ increased metabolism in lower salinity. In other words, the crustaceans and snail worked harder to transport the calcium ions they required in an environment where calcium was harder to find.

In contrast, the insects’ metabolic rates remained constant in both saline and dilute environments, even though they had a higher calcium ion transport rate in the saline environment. Insects seem to have very little demand for calcium; in fact, previous research has shown that excess calcium is potentially toxic to them.

The researchers think that the animals’ use of internal energy, or active transport, when moving the salts could be the explanation.

“When we see non-insects’ metabolisms increase in dilute environments, it could be due to the fact that they have to work harder to take in more calcium,” Buchwalter says. “And while it seems counterintuitive, the opposite is true for insects who are working harder in a more saline environment to maintain equilibrium, although their respiration rates don’t increase. Instead, they appear to utilize resources that would otherwise be dedicated to growth and development to ‘undo’ excessive ion uptake when things get saltier.

“Moving salt ions has an energy cost to the animal,” Buchwalter says. “So for freshwater insects, the idea that organisms should thrive in environments that are close to their internal salinity is wrong. Additionally, their low demand for calcium may help them thrive in very dilute environments where insects typically dominate the ecology. In contrast, low calcium appears to be stressful for the crustaceans and snail in this study. It is fascinating that species living in the same habitats can have such different physiologies.”

Future work will explore whether these physiological differences are based on the ancestry of the organisms tested, or the use of calcium in their exoskeletons/shells.

The work appears in the Journal of Experimental Biology and was supported by the National Science Foundation under grant IOS 1754884. First author and Ph.D. candidate Jamie Cochran was supported by a Goodnight Doctoral Fellowship. Catelyn Banks, formerly a student at the North Carolina School of Science and Mathematics, also contributed to the work.