Effect of carbonate ion concentration and irradiance on calcification
in planktonic foraminifera
Bemis, et al., discuss this problem on page 152: «Non-equilibrium d18O values
in planktonic foraminifera have never been adequately explained.
The annual average SST proxy used δ18O
in planktonic foraminifera in a radiocarbon - dated 1990 Bermuda Rise box core.
We report variations
in planktonic foraminifera from varved sediments off southern California spanning the past 1400 years.
Ecology of marine protists, including adaptation of protists to extreme cold; photosymbiotic associations
in planktonic foraminifera and radiolaria; pathogens and parasites of marine animals and humans; antibiotic resistance in marine animals.
Not exact matches
I was struck by the similarities between the pasta shapes shown
in Richard Webb's article on their mathematical interpretation (15 October, p 48) and some shells of
foraminifera, a type of single - celled marine
planktonic animal.
In a study published in Science in June, paleoceanographer Bärbel Hönisch and colleagues at Columbia University examined the remnants of planktonic foraminifera — single - celled creatures with elaborate shells — buried beneath the seafloor off the coast of Afric
In a study published
in Science in June, paleoceanographer Bärbel Hönisch and colleagues at Columbia University examined the remnants of planktonic foraminifera — single - celled creatures with elaborate shells — buried beneath the seafloor off the coast of Afric
in Science
in June, paleoceanographer Bärbel Hönisch and colleagues at Columbia University examined the remnants of planktonic foraminifera — single - celled creatures with elaborate shells — buried beneath the seafloor off the coast of Afric
in June, paleoceanographer Bärbel Hönisch and colleagues at Columbia University examined the remnants of
planktonic foraminifera — single - celled creatures with elaborate shells — buried beneath the seafloor off the coast of Africa.
Using Mg / Ca paleothermometry from the
planktonic foraminifera Globigerinoides ruber from the past 500 k.y. at Ocean Drilling Program (ODP) Site 871
in the western Pacific warm pool, we estimate the tropical Pacific climate sensitivity parameter (λ) to be 0.94 — 1.06 °C (W m − 2) − 1, higher than that predicted by model simulations of the Last Glacial Maximum or by models of doubled greenhouse gas concentration forcing.
Planktonic foraminifera are typically less than 0.1 mm
in diameter.
Using Mg / Ca paleothermometry from the
planktonic foraminifera Globigerinoides ruber from the past 500 k.y. at Ocean Drilling Program (ODP) Site 871
in the western Pacific warm pool, we estimate the tropical Pacific climate sensitivity parameter (λ) to be 0.94 — 1.06 °C (W m − 2) − 1, higher than that predicted by model simulations of the Last Glacial Maximum or by models of doubled greenhouse gas concentration forcing.
The TEX86 will be further analysed
in well - dated cores from the Holocene and Pleistocene and compared with other, previously determined, SST proxies such as the UK37 ′ and the d18O of
planktonic foraminifera.
They focus on two maritime sources of proxy data: coral and individual
planktonic foraminifera (monocellular organisms that float
in seawater at various depths).
Schmidt, G.A., 1999: Forward modeling of carbonate proxy data from
planktonic foraminifera using oxygen isotope tracers
in a global ocean model.
He is interested
in palaeoclimate proxies, biotic evolution and stratigraphy, with particular emphasis on the fossil record of
planktonic foraminifera from deep sea cores.