On the potential for ocean acidification to be a general cause of ancient reef crises
about
Eutrophication, microbial-sulfate reduction and mass extinctionsThe geological record of ocean acidificationA shift in the long-term mode of foraminiferan size evolution caused by the end-Permian mass extinctionSeverity of ocean acidification following the end-Cretaceous asteroid impactTwo waves of colonization straddling the K-Pg boundary formed the modern reef fish faunaCould some coral reefs become sponge reefs as our climate changes?Predicting evolutionary responses to climate change in the sea.Organism activity levels predict marine invertebrate survival during ancient global change extinctions.Projecting coral reef futures under global warming and ocean acidification.Evolutionary diversification of reef corals: a comparison of the molecular and fossil records.Microbes and mass extinctions: paleoenvironmental distribution of microbialites during times of biotic crisis.End-Cretaceous marine mass extinction not caused by productivity collapseMacroevolutionary perspectives to environmental change.Marine extinction risk shaped by trait-environment interactions over 500 million years.Extinction intensity, selectivity and their combined macroevolutionary influence in the fossil recordEvolutionary and biogeographical implications of degraded LAGLIDADG endonuclease functionality and group I intron occurrence in stony corals (Scleractinia) and mushroom corals (Corallimorpharia).CO2 and temperature decoupling at the million-year scale during the Cretaceous Greenhouse.Impact of the Late Triassic mass extinction on functional diversity and composition of marine ecosystemsUranium isotope evidence for an expansion of marine anoxia during the end-Triassic extinctionFive hundred million years of extinction and recovery: a phanerozoic survey of large-scale diversity patterns in fishesStrengthening confidence in climate change impact scienceAdditive effects of acidification and mineralogy on calcium isotopes in Triassic/Jurassic boundary limestonesModelling the impact of pulsed CAMP volcanism on pCO2 and δ13C across the Triassic–Jurassic transitionWithin- and among-genus components of size evolution during mass extinction, recovery, and background intervals: a case study of Late Permian through Late Triassic foraminiferaSensitivities of extant animal taxa to ocean acidificationRadiolarian biodiversity dynamics through the Triassic and Jurassic: implications for proximate causes of the end-Triassic mass extinctionDivergence of seafloor elevation and sea level rise in coral reef ecosystems
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P2860
On the potential for ocean acidification to be a general cause of ancient reef crises
description
im Dezember 2010 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в грудні 2010
@uk
name
On the potential for ocean acidification to be a general cause of ancient reef crises
@en
On the potential for ocean acidification to be a general cause of ancient reef crises
@nl
type
label
On the potential for ocean acidification to be a general cause of ancient reef crises
@en
On the potential for ocean acidification to be a general cause of ancient reef crises
@nl
prefLabel
On the potential for ocean acidification to be a general cause of ancient reef crises
@en
On the potential for ocean acidification to be a general cause of ancient reef crises
@nl
P1476
On the potential for ocean acidification to be a general cause of ancient reef crises
@en
P356
10.1111/J.1365-2486.2010.02204.X
P577
2010-12-01T00:00:00Z