Anomalously low alkenone temperatures caused by lateral particle and sediment transport in the Malvinas Current region, western Argentine Basin

• Published in: Deep-sea research. Part I, Oceanographic research papers Vol. 47; no. 12; pp. 2369 - 2393
• Main Authors: Benthien, Albert, Müller, Peter J.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.12.2000; Elsevier; Pergamon Press Inc
• Subjects: Alkenones; Brazil–Malvinas Confluence; Earth sciences; Earth, ocean, space; Exact sciences and technology; Isotope geochemistry; Isotope geochemistry. Geochronology; Marine; Marine and continental quaternary; Ocean currents; Oceans; Sea-surface temperature (SST); Sediments; South Atlantic Ocean; Surface sediments; Surficial geology; Temperature; UK′37; Southwest Atlantic; South Atlantic; Argentina; Atlantic Ocean; PSW, South Atlantic, Malvinas Current; Western South Atlantic; Surface sediments; U K′ 37; Alkenones; South Atlantic Ocean; Brazil–Malvinas Confluence; Sea-surface temperature (SST); South America; bathymetric maps; particulate matters; stable isotopes; O-18/O-16; Quaternary; paleotemperature; Atlantic Ocean; upper Quaternary; nutrients; surface water; drill cores; sediment transport; modern; erosion; Alkenone; Cenozoic; Phanerozoic; Holocene; seasonal variations; ocean circulation; marine sediments
• ISSN: 0967-0637; 1879-0119
• DOI: 10.1016/S0967-0637(00)00030-3

We analysed the alkenone unsaturation ratio ( U K′ 37) in 87 surface sediment samples from the western South Atlantic (5°N–50°S) in order to evaluate its applicability as a paleotemperature tool for this part of the ocean. The measured U K′ 37 ratios were converted into temperature using the global core-top calibration of Müller et al. (1998) and compared with annual mean atlas sea-surface temperatures (SSTs) of overlying surface waters. The results reveal a close correspondence (<1.5°C) between atlas and alkenone temperatures for the Western Tropical Atlantic and the Brazil Current region north of 32°S, but deviating low alkenone temperatures by −2° to −6°C are found in the regions of the Brazil–Malvinas Confluence (35–39°S) and the Malvinas Current (41–48°S). From the oceanographic evidence these low U K′ 37 values cannot be explained by preferential alkenone production below the mixed layer or during the cold season. Higher nutrient availability and algal growth rates are also unlikely causes. Instead, our results imply that lateral displacement of suspended particles and sediments, caused by strong surface and bottom currents, benthic storms, and downslope processes is responsible for the deviating U K′ 37 temperatures. In this way, particles and sediments carrying a cold water U K′ 37 signal of coastal or southern origin are transported northward and offshore into areas with warmer surface waters. In the northern Argentine Basin the depth between displaced and unaffected sediments appears to coincide with the boundary between the northward flowing Lower Circumpolar Deep Water (LCDW) and the southward flowing North Atlantic Deep Water (NADW) at about 4000 m.