FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2801200903> ?p ?o ?g. }

• W2801200903 endingPage "121" @default.
• W2801200903 startingPage "98" @default.
• W2801200903 abstract "Microbial carbonates were major components of early Paleozoic reefs until coral-stromatoporoid-bryozoan reefs appeared in the mid-Ordovician. Microbial reefs were augmented by archaeocyath sponges for ~15 Myr in the early Cambrian, by lithistid sponges for the remaining ~25 Myr of the Cambrian, and then by lithistid, calathiid and pulchrilaminid sponges for the first ~25 Myr of the Ordovician. The factors responsible for mid–late Cambrian microbial-lithistid sponge reef dominance remain unclear. Although oxygen increase appears to have significantly contributed to the early Cambrian ‘Explosion’ of marine animal life, it was followed by a prolonged period dominated by ‘greenhouse’ conditions, as sea-level rose and CO2 increased. The mid–late Cambrian was unusually warm, and these elevated temperatures can be expected to have lowered oxygen solubility, and to have promoted widespread thermal stratification resulting in marine dysoxia and hypoxia. Greenhouse conditions would also have stimulated carbonate platform development, locally further limiting shallow-water circulation. Low marine oxygenation has been linked to episodic extinctions of phytoplankton, trilobites and other metazoans during the mid–late Cambrian. We propose that this tendency to dysoxia-hypoxia in shallow marine environments also limited many metazoan reef-builders. In contrast, during the mid–late Cambrian, the ability of lithistid sponges to withstand low oxygen levels allowed them to create a benthic association with microbial carbonates that dominated global reefs. These conditions ameliorated during the Ordovician, as temperature decline promoted ocean ventilation. The prolonged time gap occupied by low diversity reefs between the ‘Cambrian Explosion’ and the ‘Great Ordovician Biodiversification Event’ reflects elevated temperatures and reduced marine oxygenation that limited metazoan diversification in shallow marine environments." @default.
• W2801200903 created "2018-05-17" @default.
• W2801200903 creator A5007103526 @default.
• W2801200903 creator A5043067545 @default.
• W2801200903 date "2018-06-01" @default.
• W2801200903 modified "2023-10-01" @default.
• W2801200903 title "Marine oxygenation, lithistid sponges, and the early history of Paleozoic skeletal reefs" @default.
• W2801200903 cites W1033374690 @default.
• W2801200903 cites W1507201230 @default.
• W2801200903 cites W1560828235 @default.
• W2801200903 cites W1562948698 @default.
• W2801200903 cites W1569011287 @default.
• W2801200903 cites W1753926244 @default.
• W2801200903 cites W1837622454 @default.
• W2801200903 cites W1896030948 @default.
• W2801200903 cites W1918983804 @default.
• W2801200903 cites W1931162404 @default.
• W2801200903 cites W1964762739 @default.
• W2801200903 cites W1965359701 @default.
• W2801200903 cites W1965646833 @default.
• W2801200903 cites W1977488297 @default.
• W2801200903 cites W1977990865 @default.
• W2801200903 cites W1980361534 @default.
• W2801200903 cites W1981457856 @default.
• W2801200903 cites W1981511174 @default.
• W2801200903 cites W1983181335 @default.
• W2801200903 cites W1983193013 @default.
• W2801200903 cites W1983309601 @default.
• W2801200903 cites W1985565047 @default.
• W2801200903 cites W1986063931 @default.
• W2801200903 cites W1986465667 @default.
• W2801200903 cites W1986730846 @default.
• W2801200903 cites W1988323425 @default.
• W2801200903 cites W1988780070 @default.
• W2801200903 cites W1988966899 @default.
• W2801200903 cites W1989822374 @default.
• W2801200903 cites W1990557336 @default.
• W2801200903 cites W1990562857 @default.
• W2801200903 cites W1990793721 @default.
• W2801200903 cites W1993018878 @default.
• W2801200903 cites W1994160943 @default.
• W2801200903 cites W1995517172 @default.
• W2801200903 cites W1996758006 @default.
• W2801200903 cites W1997065722 @default.
• W2801200903 cites W1997713847 @default.
• W2801200903 cites W1998090451 @default.
• W2801200903 cites W1999486810 @default.
• W2801200903 cites W2001812667 @default.
• W2801200903 cites W2002121443 @default.
• W2801200903 cites W2004279779 @default.
• W2801200903 cites W2004558999 @default.
• W2801200903 cites W2004722069 @default.
• W2801200903 cites W2004940647 @default.
• W2801200903 cites W2005298615 @default.
• W2801200903 cites W2005555793 @default.
• W2801200903 cites W2005750825 @default.
• W2801200903 cites W2006324634 @default.
• W2801200903 cites W2009022027 @default.
• W2801200903 cites W2010370048 @default.
• W2801200903 cites W2011440133 @default.
• W2801200903 cites W2012081789 @default.
• W2801200903 cites W2012437090 @default.
• W2801200903 cites W2014038868 @default.
• W2801200903 cites W2014734456 @default.
• W2801200903 cites W2014781455 @default.
• W2801200903 cites W2015124636 @default.
• W2801200903 cites W2015444989 @default.
• W2801200903 cites W2016049452 @default.
• W2801200903 cites W2017164848 @default.
• W2801200903 cites W2018544633 @default.
• W2801200903 cites W2023612941 @default.
• W2801200903 cites W2024148290 @default.
• W2801200903 cites W2024354120 @default.
• W2801200903 cites W2024375771 @default.
• W2801200903 cites W2024694476 @default.
• W2801200903 cites W2025261676 @default.
• W2801200903 cites W2025696977 @default.
• W2801200903 cites W2025841036 @default.
• W2801200903 cites W2028214798 @default.
• W2801200903 cites W2028456547 @default.
• W2801200903 cites W2028823240 @default.
• W2801200903 cites W2028832202 @default.
• W2801200903 cites W2029039279 @default.
• W2801200903 cites W2029054089 @default.
• W2801200903 cites W2029322624 @default.
• W2801200903 cites W2029537332 @default.
• W2801200903 cites W2030426827 @default.
• W2801200903 cites W2030474253 @default.
• W2801200903 cites W2031670040 @default.
• W2801200903 cites W2032752559 @default.
• W2801200903 cites W2033521641 @default.
• W2801200903 cites W2035577800 @default.
• W2801200903 cites W2036616803 @default.
• W2801200903 cites W2037157077 @default.
• W2801200903 cites W2037467250 @default.
• W2801200903 cites W2037469619 @default.
• W2801200903 cites W2037630861 @default.
• W2801200903 cites W2039260686 @default.

• next