Мөхөх дөхсөн эртний амьтдын бүлгүүд шинэ бүлгүүдтэй зэрэгцэн оршиж байсныг Паха формацын чулуужсан олдворууд харуулжээ.
Канадын Макгиллийн их сургууль болон Centro de Investigaciones Paleontológicas-ийн судлаачид Колумбын төв хэсэгт орших Паха формацын олдворуудыг судлахдаа Юрийн галавын үеэс үлдсэн бүлгүүд Цэрдийн галавын шинэ бүлгүүдтэй зэрэгцэн амьдарч байсныг тогтоожээ. Судалгаанд эрт Цэрдийн галавын үеийн, Вилья-де-Лейва орчмын чулуужсан олдвороор баялаг бүс нутгийг хамруулсан байна.
Макгиллийн их сургуулийн биологийн профессор Ханс Ларссон, докторын зэрэг хамгаалсан Дирли Кортес нар ийм шилжилтийг “биотын эргэлтийн цэг” хэмээх ойлголтоор тайлбарлах санал дэвшүүлжээ. Энэ нь мөхөх дөхсөн хуучин бүлгүүд шинэ бүлгүүд тэлж, төрөлжиж эхлэх үед зэрэгцэн орших хувьслын үеийг хэлнэ. Дулаан уур амьсгал, далайн түвшний өндөр байдал, шим тэжээлээр баялаг эргийн ус болон Номхон далайн зүүн хэсгийг Атлантын эхэн үеийн далайтай холбосон шинэ усан замууд энэ олон янз байдлыг дэмжсэн байж болзошгүй гэж судлаачид үзэж байна.
Паха формацын олдворуудад урт хүзүүт плезиозавр зэрэг аварга далайн мөлхөгчид, далайн матрын төрөл садан, яст мэлхий, акул, хавч хэлбэртэн багтдаг. Эдгээр амьтад нийлж Паха биотыг бүрдүүлсэн бөгөөд өмнөх судалгаагаар тэдний хоол тэжээлийн холбоог сэргээхэд дээд түвшний махчин амьтдын төрөл олон, хүнсний сүлжээ нь нарийн төвөгтэй байжээ.
Энэ олдворууд хувьслын томоохон шилжилт заавал бөөнөөр устах үйл явцтай давхцахгүй, харин мөхөж буй болон шинээр дэлгэрч буй бүлгүүдийн олон янз байдал зэрэгцэн нэмэгдэх үед ч тохиолдож болохыг харуулж байна. Гэхдээ ийм хэв маяг Дэлхийн түүхэнд хэр түгээмэл байсныг тогтоохын тулд илүү олон олдвор, чулуужсан зүйлийн насыг нарийвчлан тогтоох судалгаа, бусад бүс нутгийн формацтай харьцуулалт шаардлагатай.
Дэлгэрэнгүйг эх сурвалжаас харах
↓Эх сурвалжийг нээх ↓
An extraordinary collection of fossils in central Colombia is revealing a surprising chapter in Earth’s evolutionary history. Researchers have uncovered evidence of a time when ancient animal groups that were approaching extinction lived alongside newer groups that would eventually flourish. The discovery suggests that major evolutionary transitions can occur without the widespread destruction associated with mass extinctions.
Scientists from McGill University and the Centro de Investigaciones Paleontológicas (CIP) identified this unusual pattern while studying fossils from Colombia’s Paja Formation. The ancient marine ecosystem preserves an exceptional mixture of surviving Jurassic lineages and emerging Cretaceous groups, offering a rare glimpse into a period of profound biological change.
Drawing on these findings, McGill biology professor Hans Larsson and PhD graduate Dirley Cortés have proposed a new concept called a “Biotic Inflection.” The term describes an evolutionary turning point when older groups nearing extinction coexist with newer lineages that are beginning to expand and diversify.
A Perfect Storm for Ancient Ocean Biodiversity
The researchers believe an unusual combination of environmental conditions helped make this remarkable coexistence possible. Warm greenhouse temperatures, elevated sea levels, and coastal waters rich in nutrients may have supported an unusually diverse range of marine life.
Another important factor was the emergence of new ocean connections between the eastern Pacific and the early Atlantic through the region that is now Colombia. Together, these conditions likely created opportunities for different groups of animals to thrive within the same ecosystem. Many of these environmental influences continue to shape biodiversity around the world today.
“The Paja Formation records an extraordinary process in the history of life, when a ‘perfect storm’ of environmental factors we know to promote ecological complexity coincided with ancient lineages that were about to disappear. At the same time, new groups were beginning to flourish,” Larsson said.
A Lost World of Giant Marine Reptiles and Predators
The evidence comes from the Early Cretaceous Paja Formation near Villa de Leyva, Colombia. This fossil-rich region has preserved an astonishing variety of prehistoric marine animals, providing scientists with an unusually detailed picture of an ancient ocean ecosystem. Most of the fossils collected from the formation are housed at the CIP.
“This geological formation has produced an exceptionally rich fossil record that includes giant marine reptiles like long-necked plesiosaurs and marine crocodile relatives, as well as turtles, sharks, crustaceans and others,” Cortés explained. “Together, these animals formed the Paja Biota, one of the most ecologically complex marine communities found to date.”
In a previous study, the researchers reconstructed the feeding relationships among animals in the Paja Biota. Their analysis revealed an exceptionally intricate food web, with an unusually large variety of apex predators occupying the highest levels of the ecosystem.
This remarkable complexity makes the Paja Formation especially valuable for investigating how ecosystems change as older evolutionary groups decline and new ones become established.
Could This Discovery Change How Scientists Understand Evolution?
The proposed Biotic Inflection offers a potentially important new way to understand major changes in Earth’s biodiversity. Rather than being driven by a mass extinction, some evolutionary transitions may involve periods of extraordinary diversity, when declining lineages and emerging groups coexist.
However, the researchers emphasize that more evidence is needed to establish how common this pattern may have been. Additional fossil discoveries, more accurate estimates of fossil ages, and comparisons with geological formations in other parts of the world will help determine whether similar transitions occurred elsewhere in Earth’s history.
“I think we’ve discovered a new model of global biodiversity change. Now we’ll need to see just how widespread this could be in Earth’s history and how we can quantify its impacts,” Larsson said.
The research received funding from the Natural Sciences and Engineering Research Council of Canada, the Smithsonian Tropical Research Institute, the Anders Foundation, the 1923 Fund, Gregory D. and Jennifer Walston Johnson, the Fonds de recherche Nature et technologies Québec, and the McGill Biology Department Writing-Year Award 2024-2025.
