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A mid‐Holocene transition in the nitrogen dynamics of the western equatorial Pacific: Evidence of a deepening thermocline?
Author(s) -
Kienast M.,
Lehmann M. F.,
Timmermann A.,
Galbraith E.,
Bolliet T.,
Holbourn A.,
Normandeau C.,
Laj C.
Publication year - 2008
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2008gl035464
Subject(s) - holocene , thermocline , geology , oceanography , nitrate , sedimentary rock , advection , geochemistry , ecology , biology , physics , thermodynamics
Sedimentary δ 15 N records from the oligotrophic western equatorial Pacific (WEP) off Mindanao show that late Holocene sedimentary δ 15 N is substantially lower than that of the early Holocene, following a gradual >3 ‰ decrease that occurred between 7 and 3 kyrs ago. Analyses of modern 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 2 fixation. We suggest that the Holocene decrease in sedimentary δ 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.