The Northern Adriatic Ecosystem: Deep Time in a Shallow Sea
Columbia University Press, 2007 - Broj stranica: 299
The northern Adriatic Sea is transient, most recently flooded between 18,000 to 6,000 years ago following the last glacial maximum, and it will drain again with the onset of the next glacial period. Despite its youth, uniformly shallow depth, and flat sediment floor, it hosts a broad range of bottom-dwelling sea life ecologically resembling communities that have existed in the shallow sea since the Ordovician Period, some 500 million years ago.
The northern Adriatic is a natural laboratory in which to test hypotheses concerning the shift from the Paleozoic prevalence of stationary suspension-feeders living on the surface of the sediment and feeding from the overlying waters to, more recently, bottom-dwelling animals living dominantly in or actively seeking temporary refuge within the sediments of the sea floor, regardless of where they feed. Across the northern Adriatic Sea there is an ecological gradient from Paleozoic-style surface-dwelling communities in the east to "modern" communities living almost exclusively within the sediments in the west. Therefore, within the relatively small area of the northern Adriatic, there is an existing gradient similar to the profound ecological change from Paleozoic to more modern marine life.
During the early twentieth century, life at the bottom of the Adriatic was systematically sampled from the east to the west coasts, revealing the most common animals and their distribution. In this book Frank K. McKinney combines these findings with more recent, local studies to understand better the ecological structure of the Adriatic's floor. Specifically, he uses the predation, sediment textures and deposition rates, currents, and nutrients of northern Adriatic bottom communities to evaluate hypotheses concerning the conditions that drove surface-dwelling animals to seek long-term refuge within sea floor sediment.
Though the northern Adriatic has been well studied since the advent of the marine sciences, it is not widely known by paleontologists. With this volume, McKinney illuminates what this "living laboratory" can tell us about the evolution of multicellular life on Earth.
Što ljudi govore - Napišite recenziju
LongTerm Changes in Shallow Marine Life
Hypotheses About Causes of LongTerm Ecological Changes
Can the Threads Be Disentangled?
Sources of Fresh Water
Origin of the Adriatic
Present Tectonic Changes in and Around the Adriatic
Pleistocene and Holocene Sediments
Cyclicity of Pleistocene Adriatic Sedimentary Deposits
Composition of Adriatic Sediments
Narrow Eastern Belt of Sedimentation
Benthos Across the Northern Adriatic
Eastern Benthic Assemblages
Isolated Western Hard Substrata
Circulation in the Northern Adriatic
Nutrients and Pelagic Biology
Geochemical Budget of Nutrients
Northern Adriatic Relative to Other Regions in the Mediterranean
Benthic Hypoxia and Anoxia