Distribution of living benthic foraminifera in the northern Chukchi Sea

• Published in: arktos
• Main Authors: Racine, Calypso, Bonnin, Jérôme, Nam, Seung-Il, Giraudeau, Jacques, Biguenet, Maude, Dessandier, Pierre-Antoine, Kim, Jung‑Hyun
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Verlag (Germany) 2018
• Subjects: VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456; VDP::Mathematics and natural science: 400::Geosciences: 450::Sedimentology: 456; Living benthic foraminifera; Chukchi Sea; Water masses; Primary production; Sea-ice; Pacific; Arctic; Chukchi; Sea ice
• Online Access: https://hdl.handle.net/10037/13892; https://doi.org/10.1007/s41063-018-0062-y

This is a post-peer-review, pre-copyedit version of an article published in Arktos . The final authenticated version is available online at: https://doi.org/10.1007/s41063-018-0062-y . Living (Rose Bengal stained) benthic foraminifera were studied in the topmost sediments of five multi- and box cores collected on the continental shelf, upper and lower slopes, of the Chukchi Sea to provide background information on modern benthic foraminiferal distribution, useful for future studies. Sediment cores were collected during August–September 2015, when the area is seasonally ice-free. Benthic foraminiferal contents in the 63–125 µm and > 125 µm size fractions are discussed in terms of water masses distribution, and sedimentological (grain size) and organic geochemical (total organic carbon, total nitrogen, C/N ratio and δ 13 Corg) characteristics of the surface sediments. Marine organic carbon-rich clay sediments characterize the faunal microhabitats. Despite relatively high organic carbon contents, standing stocks of living benthic foraminifera are generally low, especially for the 63–125 µm size fraction. This low living stock seems to reflect post-bloom conditions in August and September in the area. The reduced supply of fresh organic carbon also affects faunal microhabitats in the sediment with a concentration of living fauna in the upper 2 cm of the sediment. Over the Chukchi Sea shelf, a relatively mixed upper sediment layer likely due to bioturbation or bio-structures induces a disturbed vertical distribution in the sediment. Corrosive Pacific-derived bottom water over the shelf likely explains the relative importance of agglutinated vs. calcareous fauna in this shallow setting. Our results suggest that, in a post-bloom context, the main environmental control on benthic foraminiferal assemblages in the Chukchi Sea is the nature of the bottom water masses.