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Synopsis This series of papers highlights research into how biological exchanges between salty and freshwater habitats have transformed the biosphere. Life in the ocean and in freshwaters have long been intertwined; multiple major branches of the tree of life originated in the oceans and then adapted to and diversified in freshwaters. Similar exchanges continue to this day, including some species that continually migrate between marine and fresh waters. The series addresses key themes of transitions, transformations, and current threats with a series of questions: When did major colonizations of fresh waters happen? What physiographic changes facilitated transitions? What organismal characteristics facilitate colonization? Once a lineage has colonized freshwater, how frequently is there a return to the sea? Have transitions impelled diversification? How do organisms adapt physiologically to changes in halohabitat, and are such adaptive changes predictable? How do marine and freshwater taxa differ in morphology? How are present-day global changes in the environment influencing halohabitat and how are organisms contending with them? The purpose of the symposium and the papers in this volume is to integrate findings at multiple levels of biological organization and from disparate fields, across biological and geoscience disciplines. 

Abstract. The Neogene and Quaternary are characterized by enormous changes in globalclimate and environments, including global cooling and the establishment ofnorthern high-latitude glaciers. These changes reshaped global ecosystems,including the emergence of tropical dry forests and savannahs that are foundin Africa today, which in turn may have influenced the evolution of humansand their ancestors. However, despite decades of research we lack long,continuous, well-resolved records of tropical climate, ecosystem changes,and surface processes necessary to understand their interactions andinfluences on evolutionary processes. Lake Tanganyika, Africa, contains themost continuous, long continental climate record from the mid-Miocene(∼10 Ma) to the present anywhere in the tropics and has longbeen recognized as a top-priority site for scientific drilling. The lake issurrounded by the Miombo woodlands, part of the largest dry tropical biomeon Earth. Lake Tanganyika also harbors incredibly diverse endemic biotaand an entirely unexplored deep microbial biosphere, and it provides textbookexamples of rift segmentation, fault behavior, and associated surfaceprocesses. To evaluate the interdisciplinary scientific opportunities thatan ICDP drilling program at Lake Tanganyika could offer, more than 70scientists representing 12 countries and a variety of scientificdisciplines met in Dar es Salaam, Tanzania, in June 2019. The teamdeveloped key research objectives in basin evolution, source-to-sinksedimentology, organismal evolution, geomicrobiology, paleoclimatology,paleolimnology, terrestrial paleoecology, paleoanthropology, andgeochronology to be addressed through scientific drilling on LakeTanganyika. They also identified drilling targets and strategies, logisticalchallenges, and education and capacity building programs to be carried outthrough the project. Participants concluded that a drilling program at LakeTanganyika would produce the first continuous Miocene–present record fromthe tropics, transforming our understanding of global environmental change,the environmental context of human origins in Africa, and providing adetailed window into the dynamics, tempo and mode of biologicaldiversification and adaptive radiations.