Dietary Shifts in the Hipparion Fauna of the Northern Black Sea Region
- 演化之聲
- Mar 14
- 5 min read
The Miocene epoch (approximately 23 to 5.3 million years ago) represents the most recent warm interval in Earth's geological history. From the late Miocene through the Pliocene (about 5.3 to 2.6 million years ago) and continuing into the Pleistocene Ice Age (about 2.6 million years ago to the present), the planet's average temperature has generally followed a long-term cooling trend. For this reason, studying Miocene ecosystems provides an important bridge for understanding how biological communities evolved during the transition from a warm world to the cooler climates that characterize the modern Earth.
In this study, researchers examined the dietary habits of mammals belonging to the Hipparion fauna that inhabited the northern Black Sea region during the late Miocene and early Pliocene. By reconstructing the feeding ecology of these animals, the study aimed to clarify how their diets differed from those of modern mammalian communities and how those differences reflected environmental change.
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