Focusing on the impact of bioerosion, this study explores how various organisms, including grazers and microborers, contribute to the degradation of marine skeletal carbonates and limestone coasts. It highlights the historical significance of these organisms, with traces found in ancient fossil carbonates. While much research has centered on tropical regions, this groundbreaking experimental study examines carbonate degradation and boring community development in cold-temperate to polar environments, providing new insights into these processes along a bathymetric gradient.
A little more than forty years has past since the concept of bioerosion was formally recognised as the biological erosion of hard materials. In that time, it has become apparent from the literature that bioerosional processes affect a wide range of biological and geological systems that cross many disciplines among the sciences. This book is dedicated to crossing those traditional disciplinary boundaries to present a united and current perspective on the pattern and process of bioerosion. The book opens with papers on the evolutionary significance of bioerosion, and subsequently ventures out to explore the remarkable diversity of bioerosive biota. From microboring bacteria to grazing echinoids, the studies use a variety of techniques ranging from field observations to sophisticated micro-computed tomography to investigate the ecological and environmental role of these organisms, including symbiotic interactions and alteration of non-carbonate substrates. The book concludes with a primer on the bioerosion bibliography website. A diverse set of two dozen articles, including case studies and extensive reviews, highlight many aspects of the growing discipline of bioerosion research, from the early Palaeozoic to the present, from the Tropics to the Arctic, and from terrestrial environments to the deep-sea.
First book on high-latitude bioerosion Review of the state of the art in high-latitude bioerosion First quantitative assessment of high-latitude bioerosion rates