A mid-Holocene transition in the nitrogen dynamics of the western equatorial Pacific: Evidence of a deepening thermocline?
| Autor: | Carlo Laj, Markus Kienast, Timothé Bolliet, Claire Normandeau, Moritz F. Lehmann, Ann Holbourn, Axel Timmermann, Eric D. Galbraith |
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| Jazyk: | angličtina |
| Rok vydání: | 2008 |
| Předmět: |
Delta
010504 meteorology & atmospheric sciences 010502 geochemistry & geophysics surface temperature 01 natural sciences chemistry.chemical_compound tropical Pacific Nitrate nitrate mindanao 14. Life underwater Holocene 0105 earth and related environmental sciences seawater Advection variability ocean Isotopes of nitrogen Sea surface temperature Geophysics Oceanography fresh water chemistry 13. Climate action General Earth and Planetary Sciences Sedimentary rock holocene Thermocline Geology El Nino |
| Zdroj: | Geophysical Research Letters (0094-8276) (Amer Geophysical Union), 2008-12, Vol. 35, N. L23610, P. 1-5 |
| Popis: | Sedimentary delta(15)N records from the oligotrophic western equatorial Pacific (WEP) off Mindanao show that late Holocene sedimentary delta(15)N is substantially lower than that of the early Holocene, following a gradual >3 parts per thousand decrease that occurred between 7 and 3 kyrs ago. Analyses of modem day nitrate isotope profiles from the same region indicate the sensitivity of the WEP N pools towards (1) the advection of (15)N-enriched nitrate from the Eastern Equatorial Pacific (EEP) by the North Equatorial Current (NEC) and the Mindanao Current in subsurface waters and, (2) at shallow depths, the input of new and (15)N-depleted nitrate through N, fixation. We suggest that the Holocene decrease in sedimentary delta(15)N reflects a diminished relative input of (15)N-enriched nitrate to the surface biota, either through an increase of regional nitrogen fixation, a change in nitrate consumption along the advective path of nitrate supply, or a decrease in the vertical Supply Of (15)N-enriched nitrate from the NEC. The latter mechanism is consistent with a Holocene deepening of the WEP nitracline/thermocline. Citation: Kienast, M., M. F. Lehmann, A. Timmermann, E. Galbraith, T. Bolliet, A. Holboum, C. Normandeau, and C. Laj (2008), A mid-Holocene transition in the nitrogen dynamics of the western equatorial Pacific: Evidence of a deepening thermocline?, Geophys. Res. Lett,, 35, L23610, doi: 10.1029/2008GL035464. |
| Databáze: | OpenAIRE |
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