Carbon export fluxes and export efficiency in the central Arctic during the record sea‐ice minimum in 2012: a joint <sup>234sup>Th/<sup>238sup>U and <sup>210sup>Po/<sup>210sup>Pb study
详细信息    查看全文
文摘
The Arctic sea-ice extent reached a record minimum in September 2012. Sea-ice decline increases the absorption of solar energy in the Arctic Ocean, affecting primary production and the plankton community. How this will modulate the sinking of particulate organic carbon (POC) from the ocean surface remains a key question. We use the <sup>234sup>Th/<sup>238sup>U and <sup>210sup>Po/<sup>210sup>Pb radionuclide pairs to estimate the magnitude of the POC export fluxes in the upper ocean of the central Arctic in summer 2012, covering time scales from weeks to months. The <sup>234sup>Th/<sup>238sup>U proxy reveals that POC fluxes at the base of the euphotic zone were very low (2&thinsp;&plusmn;&thinsp;2 mmol C m<sup>&minus;2sup> d<sup>&minus;1sup>) in late summer. Relationships obtained between the <sup>234sup>Th export fluxes and the phytoplankton community suggest that prasinophytes contributed significantly to the downward fluxes, likely via incorporation into sea-ice algal aggregates and zooplankton-derived material. The magnitude of the depletion of <sup>210sup>Po in the upper water column over the entire study area indicates that particle export fluxes were higher before July/August than later in the season. <sup>210sup>Po fluxes and <sup>210sup>Po-derived POC fluxes correlated positively with sea-ice concentration, showing that particle sinking was greater under heavy sea-ice conditions than under partially ice-covered regions. Although the POC fluxes were low, a large fraction of primary production (&gt;30%) was exported at the base of the euphotic zone in most of the study area during summer 2012, indicating a high export efficiency of the biological pump in the central Arctic.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700