Open AccessVariability of unusual distributions of alkenones in the surface waters of the Nordic seas
Author(s) -
Bendle James,
RosellMelé Antoni,
Ziveri Patrizia
Publication year - 2005
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/2004pa001025
Subject(s) - alkenone , oceanography , geology , arctic , water column , water mass , surface water , emiliania huxleyi , sea surface temperature , salinity , polar , climatology , environmental science , phytoplankton , chemistry , physics , organic chemistry , astronomy , environmental engineering , nutrient
Samples of filtered particulate organic matter (POM) were obtained during the summers of 1999 and 2000 from the surface waters of the Nordic seas to monitor the spatial distribution of long‐chain alkenones. The aim of the study was to appraise existing alkenone‐based climatic proxies in northern high latitudes. Unusually high percentages of the tetraunsaturated alkenone were measured in the polar waters of the East Greenland Current, with C 37:4 of up to 77% in 80% of sea‐ice cover. Values of percent C 37:4 across the Nordic seas showed a strong association with water mass type. Analysis of coccoliths in filters indicated that calcified Emiliania huxleyi could not be discounted as the biological precursor of alkenones in all the water masses. A combined data set of 69 samples of POM revealed a stronger correlation of percent C 37:4 to sea surface salinity (SSS; R 2 = 0.72) than to sea surface temperature (SST; R 2 = 0.50). Values of percent C 37:4 in sea surface POM were much higher than those in surficial sediments of the northern North Atlantic. To explain the discrepancy in sedimentary and surface water column percent C 37:4 , we propose that the alkenone contents in surface sediments underlying arctic and polar waters are a combination of autochthonous and allochthonous inputs of alkenones. Our results show that percent C 37:4 can be used to reconstruct the relative extension of arctic/polar water masses in the North Atlantic. However, the results prevent confirmation of percent C 37:4 as a paleo‐SSS proxy in the Nordic seas, given its multivariate nature in our data set and the decoupling between its range of values in surface waters and sediments.