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標(biāo)題: Titlebook: Coral Reefs at the Crossroads; Dennis K. Hubbard,Caroline S. Rogers,George D. Sta Book 2016 Springer Science+Business Media Dordrecht 2016 [打印本頁(yè)]

作者: 一再    時(shí)間: 2025-3-21 18:54
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作者: asthma    時(shí)間: 2025-3-21 20:31

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Submitting Your Module to CPAN,if this is insufficient to change reef-community structure or totally overtop low reef islands in the twenty-first century, the impacts on reefs and the organisms that depend on them will still?be profound. Patterns of sea-level rise have varied spatially in the past due to both local tectonics and
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Strong, Em, and Other Phrase Elementspeople and protecting shorelines from erosion. The anthropogenic causes of reef degradation are complex and operate over a broad range of scales and hierarchical levels, but accelerating climate change and its collateral impacts are currently the strongest drivers. Deleterious trends in local-scale,
作者: 夸張    時(shí)間: 2025-3-24 04:04
Strong, Em, and Other Phrase Elementsand function? Given the predicted effects of climate change, do reefs have a future? Is it possible to “manage” coral reefs for resilience? What can coral reef scientists contribute to improve protection and management of coral reefs? What insights can biologists and geologists provide regarding the
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作者: isotope    時(shí)間: 2025-3-24 16:51
,Coral Reefs at the Crossroads – An Introduction,easingly smaller and more specific disciplines, we often lose sight of important connections between physical and biological factors and how they can change over different spatial and temporal scales. As stresses on these robust yet fragile systems broaden and deepen, it is becoming increasingly imp
作者: 發(fā)起    時(shí)間: 2025-3-24 22:50
Coral Calcification and Ocean Acidification,n and understanding the mechanisms involved. Major findings along the way include the observation that carbon fixed by photosynthesis in the zooxanthellae is translocated to animal cells throughout the colony and that corals can therefore live as autotrophs in many situations. Recent research has fo
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Sponge Contributions to the Geology and Biology of Reefs: Past, Present, and Future,ed reefs in collaboration with microbes and other encrusting organisms. During the Cenozoic, sponges on reefs have assumed various accessory geological roles, including adhering living corals to the reef frame, protecting solid biogenic carbonate from bioeroders, generating sediment and weakening co
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Stability of Reef-Coral Assemblages in the Quaternary,ructure of coral reefs appears stable; coral assemblages from the same environments exhibit striking similarities in species composition and dominance on time scales of decades to hundreds of thousands years. Thus, community membership over time is commonly more stable and persistent than that expec
作者: GEN    時(shí)間: 2025-3-25 20:17
Reefs Through Time: An Evolutionary View,ent, reefs diversified, underwent extinctions many times and then diversified again. Reef-inhabiting organisms included many different groups from algae to vertebrates as well as enigmatic, extinct suprageneric taxa. Evolution of these groups continued unabated and sometimes resulted in significant
作者: ENDOW    時(shí)間: 2025-3-26 01:33
Climate Change, Ocean Chemistry, and the Evolution of Reefs Through Time,s have the taxa involved. Many of the data revealed by the geologic record are also relevant to human impacts on coral reefs today and their success moving forward. This chapter reviews the responses of reefs and reef builders to environmental changes over Earth’s history and relates this informatio
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https://doi.org/10.1007/978-1-4302-1111-2ortant that we break down artificial disciplinary barriers and ask questions that are difficult to frame from a single scientific perspective. This chapter provides a jumping-off point to examine coral reefs – sitting at both a disciplinary and a temporal crossroads.
作者: 玩笑    時(shí)間: 2025-3-27 11:21
https://doi.org/10.1007/978-1-4302-1921-7ly because of the perhaps unprecedented current rate of CO. release today. Present-day rates of climate change and ocean acidification may be higher than at any point in the geologic past, and may exceed the capacity for corals and other reef builders to tolerate or adapt to the changing environment.
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Strong, Em, and Other Phrase Elements aims of this book, the most pertinent question is how are reef-bioeroding taxa responding to environmental and ecological change, and how are they interacting with reef substrates under changing conditions. We discuss the current state of knowledge regarding variations in bioerosion rates and the w
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Strong, Em, and Other Phrase Elementse Mesozoic was dominated by sponges, corals, rudist bivalves, and algae, most of which were eliminated in the end-Cretaceous extinction event. The Cenozoic reef biotas included red algae, foraminifera, sponges, corals, various invertebrates, and fish..Throughout the Phanerozoic, these biotas were el
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Photosymbiosis in Past and Present Reefs,and protists. The modern dinoflagellate photosymbiont . occurs in a wide variety of unrelated host organisms from protists to mollusks. Molecular data indicate this genus first evolved either after the end-Cretaceous mass extinction 65?my ago or in the Early Eocene some 55?my ago. Encysted dinoflage
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