The inference is that both continents were once one single land-mass.
Index fossils are used to correlate rocks of similar age in different locations. By studying index fossils found in rock layers from different continents, scientists can determine which layers are of similar age and potentially infer how these continents were once connected. This information helps in reconstructing past continental configurations, such as during the time of Pangea.
the past.
Scientists used the types of rock found on different continents, specifically matching rock formations and fossils, to support the theory of plate tectonics. By observing similarities in rock types and structures across continents separated by vast oceans, they were able to infer that the continents were once connected and moved apart over hundreds of millions of years. This helped them understand the movement of the continents and the process of continental drift.
Large plate tectonics or the fossils had wings.
Fossils can provide information on the distribution of ancient species across different continents, which helps in reconstructing past continental positions. By comparing the similarities and differences in fossil species found on separate continents, scientists can infer the movement and interaction of tectonic plates in the past. Fossils can also reveal how environmental changes associated with plate movements influenced the evolution and distribution of species over time.
The missing word is "can." The complete sentence is: "Studying you can infer how Pangaea split into continents."
what type of dinosaur it is and its weight
Their teeth.
Scientists use evidence such as matching geological formations, fossils, and remnants of ancient climates found on separate continents to support the theory of plate tectonics. By analyzing these pieces of evidence, scientists can infer that the continents were once part of a single supercontinent called Pangaea.
Relative age of the rocks and the Paleo environment.
Pecten fossils are mostly found on the east coast of the United States.
A valid conclusion a scientist can make about fossils is that they provide evidence of past life forms and their environments. By studying the physical characteristics and locations of fossils, scientists can infer evolutionary relationships, extinction events, and changes in Earth's climate over time. Additionally, the stratigraphic context of fossils can reveal the relative ages of different species, contributing to our understanding of the history of life on Earth.