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Contributions in this collection discuss storm deposits dating from Neogene time between 23 and 1.8 million years ago, as well as the last 1.8 million years, including the Pleistocene and Holocene. As today, past hurricane events were responsible for the erosion of rocky shorelines due to the impact of storm waves, in addition to flood deposits due to heavy rainfall after big storms, resulting in landfall. The former typically resulted in coastal boulder deposits (CBDs) and the latter in coastal outwash deposits (CODs). Study locations covered by this treatment include three within the confines of Mexico’s Gulf of California and three in the northeast Atlantic Ocean, including the Canary Islands and Azores, as well as the coast of Norway. Rock types canvassed in these studies are dominated by igneous rocks that include surface flows such as andesite and basalt as well as surface exposures of plutonic rocks that originated deep below the surface such as granite and near-mantle rocks like low-grade chromite. These rock types reflect a range in rock density, which has an effect on the ability of storm waves to degrade rocky shores in the production of CBDs. The site-specific studies in this collection also share an application treating the shape of boulders resulting from shore erosion. The collection is introduced by a survey covering Neogene CODs registered in the geological literature and a concluding paper focused on the use of satellite images as a means for detecting previously unrecognized coastal storm deposits.
Research & information: general --- bibliography --- large clasts --- Miocene --- Pliocene --- rocky shore --- storm --- tsunami --- barrier boulder deposits --- hurricane storm surge --- hydrodynamic equation --- Gulf of California (Mexico) --- remote sensing --- bouldering tourism --- Iberian Peninsula --- Mediterranean --- Indonesia --- Central America --- coastal boulder deposits --- storm surge --- hydrodynamic equations --- Holocene --- Pleistocene --- MIS 5e (Marine Isotope Substage 5e) --- NE Atlantic Ocean --- storm waves --- western North America --- coastal storm deposits --- high-latitude settings --- upper pleistocene --- marine isotope substage 5e --- North Atlantic Ocean --- coastal erosion --- Marine Isotope Substage 5e --- Gulf of California --- n/a --- Kalgoorlie-Boulder (SE WA Goldfields SH51-09)
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Contributions in this collection discuss storm deposits dating from Neogene time between 23 and 1.8 million years ago, as well as the last 1.8 million years, including the Pleistocene and Holocene. As today, past hurricane events were responsible for the erosion of rocky shorelines due to the impact of storm waves, in addition to flood deposits due to heavy rainfall after big storms, resulting in landfall. The former typically resulted in coastal boulder deposits (CBDs) and the latter in coastal outwash deposits (CODs). Study locations covered by this treatment include three within the confines of Mexico’s Gulf of California and three in the northeast Atlantic Ocean, including the Canary Islands and Azores, as well as the coast of Norway. Rock types canvassed in these studies are dominated by igneous rocks that include surface flows such as andesite and basalt as well as surface exposures of plutonic rocks that originated deep below the surface such as granite and near-mantle rocks like low-grade chromite. These rock types reflect a range in rock density, which has an effect on the ability of storm waves to degrade rocky shores in the production of CBDs. The site-specific studies in this collection also share an application treating the shape of boulders resulting from shore erosion. The collection is introduced by a survey covering Neogene CODs registered in the geological literature and a concluding paper focused on the use of satellite images as a means for detecting previously unrecognized coastal storm deposits.
bibliography --- large clasts --- Miocene --- Pliocene --- rocky shore --- storm --- tsunami --- barrier boulder deposits --- hurricane storm surge --- hydrodynamic equation --- Gulf of California (Mexico) --- remote sensing --- bouldering tourism --- Iberian Peninsula --- Mediterranean --- Indonesia --- Central America --- coastal boulder deposits --- storm surge --- hydrodynamic equations --- Holocene --- Pleistocene --- MIS 5e (Marine Isotope Substage 5e) --- NE Atlantic Ocean --- storm waves --- western North America --- coastal storm deposits --- high-latitude settings --- upper pleistocene --- marine isotope substage 5e --- North Atlantic Ocean --- coastal erosion --- Marine Isotope Substage 5e --- Gulf of California --- n/a --- Kalgoorlie-Boulder (SE WA Goldfields SH51-09)
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Contributions in this collection discuss storm deposits dating from Neogene time between 23 and 1.8 million years ago, as well as the last 1.8 million years, including the Pleistocene and Holocene. As today, past hurricane events were responsible for the erosion of rocky shorelines due to the impact of storm waves, in addition to flood deposits due to heavy rainfall after big storms, resulting in landfall. The former typically resulted in coastal boulder deposits (CBDs) and the latter in coastal outwash deposits (CODs). Study locations covered by this treatment include three within the confines of Mexico’s Gulf of California and three in the northeast Atlantic Ocean, including the Canary Islands and Azores, as well as the coast of Norway. Rock types canvassed in these studies are dominated by igneous rocks that include surface flows such as andesite and basalt as well as surface exposures of plutonic rocks that originated deep below the surface such as granite and near-mantle rocks like low-grade chromite. These rock types reflect a range in rock density, which has an effect on the ability of storm waves to degrade rocky shores in the production of CBDs. The site-specific studies in this collection also share an application treating the shape of boulders resulting from shore erosion. The collection is introduced by a survey covering Neogene CODs registered in the geological literature and a concluding paper focused on the use of satellite images as a means for detecting previously unrecognized coastal storm deposits.
Research & information: general --- bibliography --- large clasts --- Miocene --- Pliocene --- rocky shore --- storm --- tsunami --- barrier boulder deposits --- hurricane storm surge --- hydrodynamic equation --- Gulf of California (Mexico) --- remote sensing --- bouldering tourism --- Iberian Peninsula --- Mediterranean --- Indonesia --- Central America --- coastal boulder deposits --- storm surge --- hydrodynamic equations --- Holocene --- Pleistocene --- MIS 5e (Marine Isotope Substage 5e) --- NE Atlantic Ocean --- storm waves --- western North America --- coastal storm deposits --- high-latitude settings --- upper pleistocene --- marine isotope substage 5e --- North Atlantic Ocean --- coastal erosion --- Marine Isotope Substage 5e --- Gulf of California --- Kalgoorlie-Boulder (SE WA Goldfields SH51-09)
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This reprint is a collection of papers on different aspects of the diversity and ecology of marine decapod crustaceans, including integrative taxonomy and genetic diversity, DNA barcoding to match larvae to adults, predator–prey interaction, coral–crab symbiosis, Sargassum–shrimp symbiosis, population dynamics of pelagic shrimps, diversity and distribution of oceanic larvae, spatial distribution of crabs, biodiversity of lobsters, and ecology of cave decapods. These contributions illustrate the variety of life forms, habitat use, and interspecific relationships exhibited by decapod crustaceans, one of the most diverse and abundant marine taxa.
Research & information: general --- Biology, life sciences --- cytochrome c oxidase subunit I (COI) --- larval dispersal --- mitochondrial genes --- molecular data --- 16S rRNA --- redescription --- Belzebub --- Lucifer --- sex ratio --- size structure --- size at first maturity --- population ecology --- symbiosis --- Sargassum shrimps --- chemical cues --- sponge shrimp --- coral cleaner shrimp --- taxonomy --- cytochrome oxidase 1 --- 16S ribosomal RNA --- association --- southwest Pacific Ocean --- ecology --- crustacean --- crab --- coral --- DNA barcoding --- Gulf of Mexico --- Caridea --- Dendrobranchiata --- Decapoda --- larval-adult matching --- life history --- decapods --- spiny lobsters --- slipper lobsters --- phyllosoma --- Caribbean Sea --- Yucatan Current --- lobster --- life cycle --- predator-prey --- food chain --- Brazil --- hermit crab --- Paguridae --- diversity --- molecular phylogeny --- species inventory --- zoogeography --- species richness --- depth preference --- cave zonation --- secondary stygobiosis --- trophic depletion --- protected species --- Cyclograpsus cinereus --- spatial distribution --- intertidal --- rocky shore --- negative binomial distribution --- n/a
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Like the bird whose death signaled dangerous conditions in a mine, the demise of animals that once flourished should give humans pause. How is our fate linked to the earth's creatures, and the cycle of flourishing and extinction? Which are the simple workings of nature's order, and which are omens of ecological disaster? Does human activity accelerate extinction? What really causes it? In an illuminating and elegantly written account of the widespread reduction of the world's wildlife, renowned paleontologist Niles Eldredge poses these questions and examines humankind's role in the larger life cycles of the earth, composing a provocative general theory of extinction.
Biodiversity. --- Ecology. --- Extinction (Biology) --- Adansonia. --- Aesthetics. --- Algae. --- American Museum of Natural History. --- American School of Classical Studies at Athens. --- Amherst College. --- Arthropod. --- Awareness. --- Bacteria. --- Basset Hound. --- Biodiversity. --- Biologist. --- Broad-billed roller. --- Brown University. --- Carnivore. --- Cenozoic. --- Comoro Islands. --- Cretaceous. --- Darwinism. --- East Africa. --- Ecological crisis. --- Ecology. --- Ecosystem. --- Endemism. --- Eocene. --- Evolution. --- Extinction event. --- Extinction. --- Flora. --- Forest floor. --- Fossil collecting. --- Future Evolution. --- Genetic diversity. --- Geologist. --- Geology. --- Giant coua. --- Global temperature. --- Guineafowl. --- Herbivore. --- Holocene extinction. --- Hominidae. --- Homo sapiens. --- Human evolution. --- Human eye. --- Ian Tattersall. --- Imagery. --- In Specie. --- Jellyfish. --- Jurassic. --- Lemur. --- Living systems. --- Longevity. --- Mammal. --- Mesite. --- Mesozoic. --- Miocene. --- Multicellular organism. --- Northern Hemisphere. --- Oligocene. --- Ordovician. --- Organism. --- Outcrop. --- Overexploitation. --- Paleocene. --- Paleontology. --- Paleozoic. --- Permian. --- Pheasant. --- Plant. --- Pleistocene. --- Quaternary extinction event. --- Quinine. --- Rainforest. --- Reason. --- Result. --- River mouth. --- Rock (geology). --- Rocky shore. --- Sediment. --- Sedimentary rock. --- Serengeti. --- Silurian. --- Speciation. --- State of the Environment. --- Stratum. --- Tanzania. --- Tenrec. --- Terrestrial animal. --- Trilobite. --- Tropical rainforest. --- Unicellular organism. --- University of London. --- University of Minnesota. --- University of Virginia. --- Vegetation. --- Vertebrate paleontology. --- Vertebrate. --- Wetland. --- Yale University. --- Year.
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