The carbon cycle connects different reservoirs of C, including life on Earth, atmospheric CO2, and economically important geological reserves of C. Much of this C is in reduced (organic) form, and is composed of complex chemical structures that reflect diverse biological activity, processes and transformations.
Lernziel
A wealth of information is held within the complex organic molecules, both in the context of the contemporary carbon cycle and its links to is other biogeochemical cycles, as well as in relation to Earth's history, the evolution of life and climate on this planet.
In this course we will learn about the role of reduced forms of carbon in the global cycle, how these forms of carbon are produced, move around the planet, and become sequestered in the geological record, and how they can be used to infer biological activity and conditions on this planet in the geologic past. The course encompasses a range of spatial and temporal scales, from molecular to global, and from the contemporary environment to earliest life.
Leistungskontrolle als Semesterkurs