|Seasonal Mg/Ca variability of N. pachyderma (s) and G. bulloides: Implications for seawater temperature reconstruction|Jonkers, L.; Jiménez-Amat, P.; Mortyn, P.G.; Brummer, G.-J.A. (2013). Seasonal Mg/Ca variability of N. pachyderma (s) and G. bulloides: Implications for seawater temperature reconstruction. Earth Planet. Sci. Lett. 376: 137-144. dx.doi.org/10.1016/j.epsl.2013.06.019
In: Earth and Planetary Science Letters. Elsevier: Amsterdam. ISSN 0012-821X, meer
Mg/Ca-temperature proxy; stable oxygen isotopes; planktonicforaminifera; sediment trap; North Atlantic
|Auteurs|| || Top |
- Jonkers, L.
- Jiménez-Amat, P.
- Mortyn, P.G.
- Brummer, G.-J.A., meer
Given the importance of high-latitude areas in the ocean-climate system, there is need for a paleothermometer that is reliable at low temperatures. Here we assess the applicability of the Mg/Ca-temperature proxy in colder waters (5-10 degrees C) by comparing for the first time the seasonal Mg/Ca and delta O-18 cycles of N. pachyderma (s) and G. bulloides using a sediment trap time-series from the northern North Atlantic. While both species show indistinguishable seasonal delta O-18 patterns that clearly track the near surface temperature cycle, their Mg/Ca are very different. G. bulloides Mg/Ca is high (2.0-3.1 mmol/mol), but varies in concert with the seasonal temperature cycle. The Mg/Ca of N. pachyderma (s), on the other hand, is low (1.1-1.5 mmol/mol) and shows only a very weak seasonal cycle. The delta O-18 patterns indicate that both species calcify in the same depth zone. Consequently, depth habitat differences cannot explain the contrasting Mg/Ca patterns. The elevated Mg/Ca in pristine G. bulloides might be due to the presence of high Mg phases that are not preserved in fossil shells. The contrasting absence of a seasonal trend in the Mg/Ca of N. pachyderma (s) confirms other studies where calcification temperatures were less well constrained. The reason for this absence is not fully known, but may include species-specific vital effects. The very different seasonal patterns of both species' Mg/Ca underscore the importance of parameters other than temperature in controlling planktonic foraminiferal Mg/Ca. Our results therefore lend further caution in the interpretation of Mg/Ca-temperature reconstructions from high northern latitudes.