TY - JOUR
T1 - Alkenones in Gephyrocapsa oceanica
T2 - Implications for studies of paleoclimate
AU - Volkman, John K.
AU - Barrerr, Stephanie M.
AU - Blackburn, Susan I.
AU - Sikes, Elisabeth L.
N1 - Funding Information: Acknowledgments-t-hWaen kA ndrewR evillf or valuablceo mments on the manuscripat nd for his help in preparingt he figures.J ohn Wilkin providedv ery usefula ssistancew ith data fitting, Barbara Molfinop rovidedin formatioonn t hee volutioonf Emilianiaa ndT om Truli and PeterS edwickp rovidedh elpfulc ommentosn the manuscript.W e thankJ ervisB ay SeaS portsf orp rovidingth eG . oceanica blooms amplea ndS uzannNe orwoodfo re xperat ssistancwe ithalgal cultureF. redP rahl,M anreenC ontea, nda na nonymourse vieweprr o-videdv eryh elpfula ndd etailedc ommentosn an earlierv ersiono f the manuscriptM. . Contei s also thankedf or providinga ccesst o unpublishedd ata.T his work was supportedb y theA ntarcticS cien-tific AdvisoryC ommitteaen dt heA ustralianR esearchC ouncil.
PY - 1995/2
Y1 - 1995/2
N2 - Emiliania huxleyi is widely regarded as the most likely source of C37C39 alkenones in present-day seawater and Recent sediments, but other sources are required to account for the presence of alkenones in sediments that predate the first occurrence of E. huxleyi about 265,000 years ago. Analysis of the lipids of a laboratory culture of the closely related marine coccolithophorid Gephyrocapsa oceanica (strain JB02) isolated from a massive bloom in Jervis Bay, eastern Australia showed that this species also synthesizes C37C39 alkenones and esters of di- and tri-unsaturated C36 fatty acids. This confirms earlier predictions based on the fossil record that species of Gephyrocapsa should contain these distinctive biomarkers. In this strain of G. oceanica the sum of the C38 ethyl ketone concentrations is similar to, or greater than, that of the C37 methyl ketones over the temperature range 11-29°C, whereas the reverse is true for Emiliania huxleyi. It should thus be possible to determine whether there is a contribution from Gephyrocapsa to the alkenones in seawater and sediments. The concentrations per cell of the major alkenones showed different responses to increasing growth temperature. The 37:3 and 38:3 methyl alkenones and 38:3 ethyl alkenone showed an approximately linear decrease in cellular concentration over the entire temperature range, whereas the 37:2 and 38:2 methyl alkenones and 38:2 ethyl alkenone concentrations showed almost no change from 11 to 20°C followed by a dramatic increase above 20°C. As a result, the ratio of di- to tri-unsaturated methyl alkenones as measured by U37k′ changes greatly with growth temperature, but the is different from that found for E. huxleyi in culture. The temperature response can be approximated by the linear relationship U37k′ = 0.049T - 0.520 (r2 = 0.89), although a better fit can be obtained using polynomial expressions. These data might account for some of the apparent anomalies in predictions of sea surface temperature (SST) derived from Emiliania-based alkenone-SST calibrations in those sediments which contain contributions from Gephyrocapsa.
AB - Emiliania huxleyi is widely regarded as the most likely source of C37C39 alkenones in present-day seawater and Recent sediments, but other sources are required to account for the presence of alkenones in sediments that predate the first occurrence of E. huxleyi about 265,000 years ago. Analysis of the lipids of a laboratory culture of the closely related marine coccolithophorid Gephyrocapsa oceanica (strain JB02) isolated from a massive bloom in Jervis Bay, eastern Australia showed that this species also synthesizes C37C39 alkenones and esters of di- and tri-unsaturated C36 fatty acids. This confirms earlier predictions based on the fossil record that species of Gephyrocapsa should contain these distinctive biomarkers. In this strain of G. oceanica the sum of the C38 ethyl ketone concentrations is similar to, or greater than, that of the C37 methyl ketones over the temperature range 11-29°C, whereas the reverse is true for Emiliania huxleyi. It should thus be possible to determine whether there is a contribution from Gephyrocapsa to the alkenones in seawater and sediments. The concentrations per cell of the major alkenones showed different responses to increasing growth temperature. The 37:3 and 38:3 methyl alkenones and 38:3 ethyl alkenone showed an approximately linear decrease in cellular concentration over the entire temperature range, whereas the 37:2 and 38:2 methyl alkenones and 38:2 ethyl alkenone concentrations showed almost no change from 11 to 20°C followed by a dramatic increase above 20°C. As a result, the ratio of di- to tri-unsaturated methyl alkenones as measured by U37k′ changes greatly with growth temperature, but the is different from that found for E. huxleyi in culture. The temperature response can be approximated by the linear relationship U37k′ = 0.049T - 0.520 (r2 = 0.89), although a better fit can be obtained using polynomial expressions. These data might account for some of the apparent anomalies in predictions of sea surface temperature (SST) derived from Emiliania-based alkenone-SST calibrations in those sediments which contain contributions from Gephyrocapsa.
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U2 - 10.1016/0016-7037(95)00325-T
DO - 10.1016/0016-7037(95)00325-T
M3 - Article
SN - 0016-7037
VL - 59
SP - 513
EP - 520
JO - Geochimica et Cosmochimica Acta
JF - Geochimica et Cosmochimica Acta
IS - 3
ER -