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100-million-year-old dinosaur eggs recovered in Jurassic America

100-million-year-old dinosaur eggs recovered in Jurassic America

Time of India05-06-2025
100-million-year-old dinosaur eggs recovered in Jurassic America
Central Utah, 100 million years ago, was a very different place–covered in forests and water. It was a lush, watery landscape on the edge of the Western Interior Seaway.
In this landscape, dinosaurs and early mammals drank from the same water sources, while ancient crocodiles hid beneath the surface, to attack their prey. Dense forests and rivers supported a wide variety of life. This region was part of a dynamic ecosystem where survival depended on constant adaptation. Recent fossil discoveries from the Mussentuchit Member of the Cedar Mountain Formation—including bones and broken eggshells—offer a rare glimpse, helping scientists understand the creatures that once thrived in this ancient, ever-changing environment.
4000 dinosaur eggshell fragments found buried in 20 sites
For over a year, paleontologists assumed that there was just one type of dinosaur egg buried in the sediments.According to earth.com, their assumption was proven wrong after the researchers collected more than 4,000 eggshell fragments from 20 sites and examined them under scanning electron microscopes and light microscopes. As the eggshells split into at least six distinct ootaxa- a scientific term for fossil egg species, showed that several different animals shared the same nesting grounds.
'The most interesting thing about this for me is the multiple types of elongatoolithid eggshells, which correspond to multiple types of oviraptorosaur dinosaurs', shared Dr. Josh Hedge, a visiting assistant professor of biology at Lake Forest College.
He added, 'I think historically we have been guilty of thinking there is one kind of each dinosaur in a given ecosystem, but we are finding more and more that multiple species of each group are likely coexisting.'
Their research suggests that at least two or three oviraptorosaurs of different sizes were laying eggs in that Utah ecosystem at the same time.
Dinosaur egg diversity
Many of the eggshells found belonged to feathered dinosaurs called Oviraptorosauras. These eggs were long and narrow, similar to the modern bird eggs, a shape that might have helped the embryos breathe while buried in warm sand. Other eggs belonged to plant eating dinosaurs that walked on two legs called Ornithopods.
But perhaps the most surprising find was Mycomorphoolithus kohringi, an egg type previously found only in Europe, indicating that a crocodylomorph, a prehistoric relative of crocodiles, also lived in North America during the Cretaceous period.
About the egg layers
Most Oviraptorosaurs were mid-sized, feathered omnivores with strong beaks and stubby tails. Among the recent skeletal finds, Moros, a horse-sized early tyrannosaur, and lani, a beaked plant-eater were also found.
Meanwhile, Ornithopods were the workhorses of the Cretaceous West. They left abundant tracks but rarely complete skeletons. They were dry-season grazers or wet-season browsers.Their thick-walled eggs support the idea that they buried their clutches in vegetation, much like today's megapode birds.
What eggs clue about the ancient ecosystem
Clutch spacing, shell thickness , and pore patterns tell us about the soil moisture, vegetation cover, and parental care behaviors.
The six ootaxa signify: shallow buried mounds for crocodile cousins, sand plastered rings for oviraptorosaurs, and leaf-blanketed pits for ornithopods.
Microscopic and scanning electron analysis revealed crystallite patterns thinner than a human hair, allowing the scientists to match tiny fragments to broader evolutionary groups.
This wide variety suggests the characteristics of an ecosystem, rich in microhabitats, where animals could partition the resources and thrive side by side.
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New study finds 117-million-year-old geological formations rewriting Atlantic Ocean history
New study finds 117-million-year-old geological formations rewriting Atlantic Ocean history

Time of India

time5 days ago

  • Time of India

New study finds 117-million-year-old geological formations rewriting Atlantic Ocean history

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When the young North Atlantic's saline waters finally breached into the long-isolated southern basins, they encountered dense, carbon-rich deep waters that had been locked away for millions of years. This sudden mixing unleashed colossal underwater mud avalanches, cascading across the seabed with immense force and reshaping the ocean floor's topography on a scale rarely seen in Earth's past. The consequences reached far beyond the geology. This tectonic–oceanic upheaval likely interrupted one of the planet's most important climate-regulating processes: the long-term burial of carbon in marine sediments. By disturbing these ancient, carbon-heavy layers, the event may have kept vast amounts of greenhouse gases circulating in the atmosphere, helping sustain the elevated global temperatures characteristic of the mid-Cretaceous, a period often referred to as one of Earth's 'greenhouse worlds.' 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Dinosaur teeth used to recreate prehistoric air for the first time
Dinosaur teeth used to recreate prehistoric air for the first time

Time of India

time06-08-2025

  • Time of India

Dinosaur teeth used to recreate prehistoric air for the first time

In a groundbreaking scientific breakthrough, researchers have successfully reconstructed the prehistoric atmosphere using fossilized dinosaur teeth . This achievement could reshape our understanding of Earth's ancient climate . Led by geochemist Dingsu Feng of the University of Göttingen, the international team analyzed oxygen isotopes preserved in the enamel of teeth from the Cretaceous and Jurassic periods. Their findings reveal not only the composition of the air dinosaurs once breathed but also hint at sudden, massive CO2 spikes likely linked to volcanic activity. The results provide a new method to study climate dynamics over deep time and understand extinction events. How dinosaur teeth preserve ancient atmospheric clues The study focused on the analysis of oxygen-17, a rare isotope that leaves behind telltale chemical signatures when inhaled by air-breathing vertebrates. Over millions of years, these signals remain preserved in durable tissues such as tooth enamel. Because teeth are less susceptible to environmental contamination, they serve as reliable time capsules of ancient biology and atmospheric conditions. Researchers examined previously collected tooth enamel powders from museum specimens across Europe, including those of Tyrannosaurus rex and Kaatedocus, a sauropod dinosaur. These samples held valuable information about oxygen ratios, which correlate with atmospheric CO2 concentrations. by Taboola by Taboola Sponsored Links Sponsored Links Promoted Links Promoted Links You May Like 15 Foods That Might Kill You Before Anything Else Does Undo CO2 levels in the age of dinosaurs Based on the isotope readings, scientists determined that atmospheric CO2 levels were far higher during the Mesozoic era than today. In the late Jurassic, CO2 concentrations reached about 1,200 parts per million (ppm). During the late Cretaceous, this figure dropped slightly to around 750 ppm. For comparison, modern atmospheric CO2 levels hover around 430 ppm. This confirms previous models suggesting that dinosaurs lived in a hotter, more carbon-rich world, largely influenced by natural processes such as plate tectonics and sustained volcanic activity. Volcanic activity and sudden climate changes A particularly fascinating discovery was the spike in isotope anomalies in two specific teeth—one from a T. rex and another from a Kaatedocus. These anomalies suggest short-lived but significant surges in atmospheric CO2. Scientists believe these may be linked to massive volcanic eruptions, such as flood basalt events, which released enormous amounts of CO2 in a short geological timeframe. Such findings support the idea that volcanic CO2 emissions played a major role in driving rapid climate changes, which may have affected ecosystems and evolutionary pressures on land-dwelling vertebrates. Implications for modern climate science The ability to reconstruct prehistoric air with such precision opens new doors for understanding both past and future climate patterns. By identifying CO2 fluctuations during the age of dinosaurs, researchers can refine models that predict how modern ecosystems might respond to accelerated carbon emissions. This study also highlights the potential of fossilized remains as archives of environmental data, giving scientists tools to trace how life and climate have co-evolved over hundreds of millions of years. Next target: The Great Dying Buoyed by their success, the team now plans to apply the same method to fossils from the Permian-Triassic extinction event, known as the Great Dying, which occurred 252 million years ago. This catastrophic period saw the extinction of over 90% of marine species and 70% of terrestrial life, likely due to prolonged volcanic eruptions in what is now Siberia. By analyzing teeth from this period, researchers hope to uncover how atmospheric CO2 behaved before, during, and after this global extinction, offering new clues into Earth's resilience and recovery mechanisms. From volcanic eruptions to global extinction events, dinosaur teeth have revealed more than just what these creatures ate. They've opened a window into the very air they breathed. This pioneering research underscores the power of modern geochemistry and paleontology to unravel the secrets of Earth's deep past, with implications that stretch far into the planet's uncertain climatic future.

Researchers Study Prehistoric CO2 Levels After Reconstructing Air From Dinosaur Teeth
Researchers Study Prehistoric CO2 Levels After Reconstructing Air From Dinosaur Teeth

NDTV

time05-08-2025

  • NDTV

Researchers Study Prehistoric CO2 Levels After Reconstructing Air From Dinosaur Teeth

Researchers have analysed the oxygen isotope ratios in fossilised dinosaur teeth, specifically the tooth enamel. The tooth has preserved traces of the ancient atmosphere. The researchers studied these isotopes to understand atmospheric CO2 levels during the Mesozoic era, when dinosaurs roamed the Earth. The CO2 levels were much higher during that time, with concentrations reaching up to 1,200 parts per million in the late Jurassic and 750 parts per million in the late Cretaceous. To understand it better, today's atmospheric CO2 levels are around 430 parts per million. The volcanic activity apparently played a significant role in shaping the prehistoric atmosphere. According to the researchers, some dinosaur teeth showed signs of high CO2 levels likely caused by large flood basalt eruption events. "Our findings provide a new research avenue to reconstruct a direct link between land-living vertebrates and the atmosphere they breathed," palaeontologist and geochemist Thomas Tutken of the Institute of Geosciences at Johannes Gutenberg Universitat, Mainz in Germany, told Science Alert. "Even after up to 150 million years, isotopic traces of the oxygen molecules of the Mesozoic atmosphere that the dinosaur inhaled are still preserved in fossil tooth enamel and can tell us something about the ancient atmosphere composition and global photosynthetic biomass production." Now, the team plans to apply this method to other geological periods, including the Permian-Triassic extinction event, to understand the Earth's climate history better. This innovative approach has shed new light on the prehistoric atmosphere and has the potential to revolutionise our understanding of Earth's climate history. "Overall, triple oxygen isotope analysis of fossil teeth of terrestrial amniotes can provide insights into past atmospheric greenhouse gas content and global primary productivity," the researchers wrote in the study.

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