Study Reveals How Dinosaurs’ Free-Range Parenting Transformed the Mesozoic Era

University of Maryland paleontologist Thomas R. Holtz Jr. has explored how dinosaurs adapted to their ancient environments and the differences between those worlds and our own for decades. His recent research suggests that crucial factors may have been overlooked in comparing ancient dinosaurs with modern mammals.

Some sauropod dinosaurs, Alamosaurus sanjuanensis, formed herds divided by age. Image credit: DiBgd.

“Many people view dinosaurs as the Mesozoic equivalent of mammals since both groups were the dominant land animals of their respective eras,” says Holtz.

“However, a crucial difference relates to their reproductive and child-rearing strategies, which scientists haven’t fully considered when comparing these worlds.”

“The methods by which animals raise their young significantly influence their ecosystems. Understanding these differences can help scientists reevaluate ecological diversity,” he explains.

“Young mammals often receive extensive care from their mothers until they are nearly fully grown.”

“In essence, mammal offspring fulfill similar ecological roles as their parents; they consume similar food and interact within the same environment because adults handle most of the responsibilities.”

“You could say mammals have ‘helicopter’ parents—particularly helicopter mothers,” he continues.

“For example, mother tigers continue to hunt for cubs that are nearly their size.”

“Even young elephants, among the largest animals in the Serengeti at birth, rely on their mothers for years.”

“Humans exhibit similar behavior, caring for our children until they reach adulthood.”

“Conversely, dinosaurs exhibited different parenting behaviors. They offered some parental care, but their young were relatively independent.”

“After a short period, from a few months to a year, young dinosaurs left their parents to roam independently, often cautious of one another.”

Dr. Holtz notes that adult crocodiles, closely related to dinosaurs, demonstrate a similar trend.

Crocodiles guard their nests and protect their young for a limited duration; however, within a few months, the young disperse and lead independent lives, taking years to reach adulthood.

“Dinosaurs could be likened to ‘latchkey kids,'” Holtz states.

“Fossil evidence shows that juvenile skeletons were often found together, with no adults nearby.”

“These juveniles congregated in groups of similar ages, learning to feed themselves and fend for their safety.”

This parenting style suited the fact that dinosaurs laid eggs and produced relatively large chicks at once.

By producing multiple offspring at a time and reproducing more frequently than mammals, dinosaurs increased the chances of their lineage’s survival without significant resource investment.

“The key takeaway is that this early separation between parents and offspring, alongside size differences, likely had significant ecological implications,” Holtz noted.

“The dietary needs of dinosaurs shifted as they matured, as did their vulnerabilities to predators and their mobility.”

“Even though adult and juvenile dinosaurs belong to the same biological species, they occupy distinctly different ecological niches.”

“Therefore, they can be regarded as different ‘functional species.’

For instance, a juvenile Brachiosaurus, comparable in size to a sheep, couldn’t access food 10 meters above ground like its adult counterparts.

Juveniles faced different predators, feeding in different locations and avoiding fully grown adults.

As young Brachiosaurus grow from dog-sized to horse-sized to giraffe-sized, their ecological roles evolve significantly.

“This understanding has transformed how scientists perceive ecological diversity,” Holtz emphasized.

Typically, scientists argue that modern mammals inhabit more diverse ecosystems because of the coexistence of varied species.

However, if young dinosaurs are counted as separate functional species and their numbers recalculated, the total functional species in dinosaur fossil assemblages likely exceeds that of mammalian fossil assemblages.

How did ancient ecosystems accommodate all these functional roles? Dr. Holtz proposes two potential explanations.

First, the Mesozoic era featured unique environmental conditions, such as warmer temperatures and elevated carbon dioxide levels.

These factors likely enhanced plant productivity, generating more food energy to sustain larger populations.

Secondly, dinosaurs may have had lower metabolic rates than similarly sized mammals, demanding less food for survival.

“Our world might actually be less productive in terms of plant resources than the age of dinosaurs,” claims Holtz.

“A more robust food chain could support greater functional diversity.”

“If dinosaurs’ physiological demands were lower, their ecosystems might have accommodated far more functional species than found in mammalian systems.”

Dr. Holtz emphasizes that his theory doesn’t necessarily imply that dinosaur ecosystems were vastly more diverse than those of mammals, but rather that diversity may have existed in forms that have yet to be identified by scientists.

He intends to further explore similar patterns within the context of dinosaur functional diversity across different life stages to gain deeper insights into their world and its evolution into our contemporary ecosystem.

“We shouldn’t merely consider dinosaurs as scaled and feathered versions of mammals,” Holtz concludes.

“They are remarkable creatures in their own right, and the full scope of their existence is still being uncovered.”

This research will be detailed in Holtz’s paper, set to appear in the Italian Journal of Geosciences.

_____

Thomas R. Holtz Jr. et al. 2026. Raising Babies: A Preliminary Investigation into Ontogenetic Niche Partitioning in Dinosaurs and Long-term Maternal Care in Mammals within Their Ecosystems. Italian Journal of Geosciences 145; doi: 10.3301/IJG.2026.09

Source: www.sci.news

Scientists Uncover Mesozoic Carbon Dioxide Levels and Photosynthesis Through Dinosaur Tooth Enamel Analysis

During the Mesozoic era, from 252 to 66 million years ago, analyses of the oxygen isotope composition in dinosaur teeth revealed that the atmosphere contained significantly more carbon dioxide than it does today, with global plant photosynthesis levels roughly double those of the present.



Fossil teeth of Camarasaurus from the Morrison Formation in the US. Image credit: sauriermuseum aathal.

A study conducted by Göttingen University and researcher Dr. Dingsu Feng examined the dental enamel of dinosaurs that roamed North America, Africa, and Europe during the Late Jurassic and Late Cretaceous periods.

“Enamel is one of the most stable biological materials,” they explained.

“It captures different oxygen isotopes based on the air dinosaurs inhaled with each breath.”

“The isotope ratios of oxygen reflect fluctuations in atmospheric carbon dioxide and plant photosynthesis.”

“This connection allows us to infer insights about the climate and vegetation of the dinosaur era.”

“During the late Jurassic, about 150 million years ago, the air contained four times more carbon dioxide than before industrialization, prior to significant human emissions of greenhouse gases.”

“In the late Cretaceous, around 730 to 66 million years ago, carbon dioxide levels were three times higher than today.”

Teeth from two dinosaur species, the Tyrannosaurus Rex and Kaatedocus siberi, showed an exceptionally unique oxygen isotope composition.

This phenomenon is indicative of carbon dioxide spikes linked to major geological events like volcanic eruptions—such as the massive eruption of the Deccan Traps in India at the close of the Cretaceous period.

The heightened photosynthetic activity of plants at that time on both land and water is likely associated with elevated carbon dioxide levels and higher average annual temperatures.

This research marks a milestone in paleoclimatology. Historically, soil and marine proxy carbonates have served as the primary tools for reconstructing past climates.

Marine proxies, which are indicators of sediment fossils and chemical signatures, help scientists comprehend ancient marine environmental conditions, yet these methods often involve uncertainties.

“Our approach offers a fresh perspective on the planet’s history,” Dr. Fenn remarked.

“It paves the way to use fossilized tooth enamel for probing the composition of Earth’s atmosphere and plant productivity during that era.”

“Understanding these factors is crucial for grasping long-term climate dynamics.”

“Dinosaurs may well become new climate scientists, as their teeth have recorded climate data for over 150 million years. At last, we have received their message.”

Study published on August 4, 2025, in Proceedings of the National Academy of Sciences.

____

Dingsu Feng et al. 2025. Mesozoic Atmospheric CO2 Concentrations reconstructed from the enamel of dinosaur teeth. PNAS 122 (33): E2504324122; doi: 10.1073/pnas.2504324122

Source: www.sci.news

Research: Collaboration between oceans and continents led to Mesozoic marine extinctions

in paper Published in the journal Nature ChemistryScientists have proposed a new explanation for a series of severe environmental crises known as marine anoxia, which occurred between 185 and 85 million years ago (during the Mesozoic era) when the amount of dissolved oxygen in the oceans became extremely low.

Oceanic anoxia was a geologically abrupt phase of extreme oxygen depletion in the oceans that disrupted marine ecosystems and led to evolutionary shifts. These events, which usually lasted about 1.5 million years, occurred frequently during the Mesozoic Era, between about 183 and 85 million years ago. One hypothesis suggests that anoxia resulted from increased chemical weathering of the Earth's surface on a greenhouse world with high volcanic carbon emissions. Gernon othersA combination of plate reconstructions, tectonic geochemical analyses and global biogeochemical modelling tested this hypothesis. Image courtesy of the University of Southampton.

“Ocean anoxia is like hitting the reset button on the Earth's ecosystems,” said Prof Tom Gernon, from the University of Southampton.

“The challenge was to understand what geological forces pushed the button.”

The researchers investigated the influence of plate tectonic forces on ocean chemistry during the Jurassic and Cretaceous periods, collectively known as the Mesozoic Era.

“This period in Earth's history is also known as the Age of the Dinosaurs and is well exposed along the cliffs of the Jurassic Coast on the south coast of England, Whitby in Yorkshire and Eastbourne in East Sussex,” Prof Gernon said.

Scientists have combined statistical analysis and advanced computer modelling to investigate how the ocean's chemical cycle may have responded to the breakup of the supercontinent Gondwana, the giant landmass once home to dinosaurs.

“During the Mesozoic Era, the continents broke apart and intense volcanic activity occurred around the world,” Prof Gernon said.

“As the plates shifted and new ocean floor was formed, phosphorus, a nutrient essential to life, was released in large quantities into the ocean from weathered volcanic rocks.”

“Importantly, we found evidence of multiple instances of chemical weathering on both the ocean floor and the continents, alternating between destroying the oceans — like a geological tag team.”

The authors find that the timing of these weathering waves coincides with most of the marine anoxic events in the rock record.

They argue that phosphorus that entered the ocean through weathering acted as a natural fertilizer, promoting the growth of marine life.

However, this fertilization phenomenon came at a great cost to marine ecosystems.

“Increased biological activity caused huge amounts of organic matter to sink to the seafloor, consuming huge amounts of oxygen,” said Prof Benjamin Mills, from the University of Leeds.

“This process ultimately left large swaths of the ocean anoxic, or 'dead zones' where oxygen was depleted and most marine life died.”

“The anoxic conditions typically lasted for one to two million years and had profound effects on marine ecosystems, the effects of which are still felt today.”

“The organic-rich rocks that accumulated during these events are the source of the world's largest commercial oil and gas reserves to date.”

The findings explain the causes of extreme biological chaos during the Mesozoic Era and highlight the devastating effects of nutrient overload on marine environments today.

“Studying geological events provides valuable insights that help us understand how Earth will respond to future climatic and environmental stresses,” Professor Gernon said.

Overall, the results reveal stronger-than-expected connections between Earth's solid interior and its surface environment and biosphere, especially during periods of tectonic and climatic upheaval.

“It is remarkable how a series of events occurring inside the Earth can have such profound, often devastating, effects on the surface,” Prof Gernon said.

“Continental breakup could have profound effects on evolutionary processes.”

_____

TM Gernon othersSolid Earth forcing of Mesozoic oceanic anoxia. National GeographyPublished online August 29, 2024, doi: 10.1038/s41561-024-01496-0

This article has been adapted from an original release from the University of Southampton.

Source: www.sci.news