A small, dagger-shaped fossil — about 33–46 cm long and heavily mineralised — pulled from river gravels along the Sahansara in Uttar Pradesh has set off a flurry of excitement among local researchers. The specimen, first flagged by Dehradun-based palaeo-environmentalist Dr Umar Ali Saif and sent to expert groups for study, appears to be the nasal horn of a horned (ceratopsian) dinosaur that resembles the famous three-horned Triceratops. While the identification remains provisional, the find has sparked excitement because horn-cores of ceratopsian dinosaurs like Triceratops have not been previously documented in the Indian subcontinent’s foothill deposits. Scientists caution that rigorous lab tests and comparisons are needed, but the find is already being called “potentially ground-breaking” for Indian palaeontology.
The fossil in question was found in sediments along the Sahansara River, which drains portions of the Shivalik foothills. The fragment, reported to be about 33–46 cm in length and 4–5.5 cm thick with a pointed tip of roughly 8 cm, seems to match the proportions of nasal-horn cores of horned dinosaurs. It is described as having been deeply mineralised and converted into sandstone after burial in the foothills, with an estimated age of approximately 35-40 million years (though precise dating is pending).
Because horned-dinosaur elements such as those from Triceratops are mostly known from Late Cretaceous deposits in western North America, finding a similar fossil in northern India’s Shivalik terrain is unexpected. The sediment context and depositional history of the site will need detailed study in order to understand whether the fossil can be assigned to Triceratops, a close relative, or a different horned-dinosaur lineage altogether.
The dinosaur genus Triceratops, meaning “three-horned face,” is one of the most recognisable ceratopsian dinosaurs. It was a large quadrupedal herbivore, up to about 7-9 metres long, bearing a large bony frill at the back of its skull, two long brow horns above the eyes, and a shorter horn above the beak. Triceratops lived during the Late Cretaceous epoch, roughly between 68 and 66 million years ago.
In contrast, the fossil from Saharanpur sits in a geological environment where horned dinosaur remains have not been robustly documented. Much of India’s dinosaur fossil record comes from Late Cretaceous sediments such as the Lameta Formation and from western/central India; horned dinosaurs like Triceratops have not been reliably recorded in the north-western Shivalik foothills. Published surveys of Indian dinosaur-fossil records note that fluvial and lacustrine terrestrial sediments conducive to dinosaur preservation are relatively rare in many parts of the subcontinent. In other Indian localities, more dinosaur evidence has been found—such as nesting sites of titanosaurs in the Narmada Valley, where 92 fossil nesting sites bearing 256 eggs were identified, suggesting complex reproductive behaviours among large herbivorous dinosaurs.
If the Saharanpur fragment does turn out to be a nasal horn of a Triceratops-type dinosaur, it suggests either an as-yet-undocumented dispersal of ceratopsians into the Indian subcontinent or a convergent evolution of horn structures in local dinosaur lineages. Either possibility would invite major re-thinking of dinosaur biogeography in Cretaceous Gondwanan-derived landmasses.
While horned-ceratopsian dinosaurs remain unconfirmed in the Shivalik region, there is a record of other dinosaurs and vertebrate fossils in adjoining areas:
In central India’s Narmada Valley, researchers uncovered 92 nesting sites containing a total of 256 fossil eggs attributed to titanosaurs, large sauropod herbivores of the Late Cretaceous.
Broad reviews of Indian dinosaur fossil records indicate that most finds date to the Maastrichtian stage of the Late Cretaceous, and that the Indian record is comparatively patchy due to limited suitable sedimentary basins.
Fossil parks in the Shivalik region (for example, in Himachal Pradesh) document later-period vertebrate fossils (mammals, tortoises, rhinos) from the Plio-Pleistocene rather than classic dinosaurs.
These records show that the broader region does have fossil-yielding stratigraphy, though classic horned dinosaur remains like those of Triceratops are not yet part of the documented Indian fauna.
The fossil fragment from Saharanpur is an intriguing and potentially landmark discovery but remains provisional until further scientific work is completed. The next steps will include: morphological comparison with known ceratopsian horn cores, stratigraphic analysis of the sedimentary context, radiometric or isotopic dating of the host rock, and broader field survey in the area to search for associated bones or teeth. If confirmed, this find would extend the known range of three-horned dinosaur types into India, shed new light on Late Cretaceous dinosaur dispersal, and underscore the Shivalik foothills as a potentially richer fossil frontier than previously recognised. Until then, the fossil remains a compelling possibility and a call for deeper palaeontological exploration in the region.
(With inputs from various sources.)
1. What fossil was found in Saharanpur, Uttar Pradesh?
Researchers discovered a horn-shaped fossil along the Sahansara River that closely resembles the nasal horn of a Triceratops-type dinosaur, potentially the first of its kind in India.
2. Why is the Saharanpur fossil discovery significant?
If confirmed, this fossil could be India’s first evidence of a horned ceratopsian dinosaur, suggesting new insights into dinosaur evolution and dispersal across ancient Gondwana landmasses.
3. What is a Triceratops?
Triceratops was a large, three-horned herbivorous dinosaur that lived about 68–66 million years ago during the Late Cretaceous. It is one of the most recognizable dinosaurs in the world.
4. Have Triceratops fossils been found in India before?
No. Until now, horned dinosaurs like Triceratops were only known from North America. This find, if verified, would be the first evidence of such a species in the Indian subcontinent.
5. Where was the Saharanpur fossil found and how old is it?
The fossil was found in river sediments along the Sahansara in the Shivalik foothills. Preliminary estimates suggest it could be around 35–40 million years old, pending detailed analysis.