The oceanic biological pump: Rapid carbon transfer to depth at continental margins during winter
| dc.contributor.author | Thomsen, Laurenz | |
| dc.contributor.author | Aguzzi, Jacopo | |
| dc.contributor.author | Costa, Corrado | |
| dc.contributor.author | De Leo, Fabio | |
| dc.contributor.author | Ogston, Andrea | |
| dc.contributor.author | Purser, Autun | |
| dc.date.accessioned | 2019-01-24T17:47:43Z | |
| dc.date.available | 2019-01-24T17:47:43Z | |
| dc.date.copyright | 2017 | en_US |
| dc.date.issued | 2017 | |
| dc.description.abstract | The oceanic biological pump is responsible for the important transfer of CO2-C as POC “Particulate Organic Carbon” to the deep sea. It plays a decisive role in the Earth’s carbon cycle and significant effort is spent to quantify its strength. In this study we used synchronized daily time-series data of surface chlorophyll-a concentrations from the NASA’s MODIS satellite in combination with hourly to daily observations from sea surface buoys and from an Internet Operated Vehicle (IOV) on the seafloor within Barkley Canyon (Northeast Pacific) to investigate the importance of winter processes in the export of fresh phytodetritus. The results indicate that phytoplankton pulses during winter can be as important in POC transfer to depth as the pulses associated with spring and summer blooms. Short winter phytoplankton pulses were observed to disappear from surface waters after low-pressure systems affected the area. Pulses of chlorophyll reached the IOV, at 870 m depth on the canyon seafloor, 12–72 hours later. These observed short pulses of biological carbon production regularly observed in the region from December to March have not been considered a significant component of the biological pump when compared with the denser summer productivity blooms. | en_US |
| dc.description.reviewstatus | Reviewed | en_US |
| dc.description.scholarlevel | Faculty | en_US |
| dc.description.sponsorship | This work was supported by Ocean Networks Canada. The development of the IOV was supported by the European Commission and the ROBEX Helmholtz Alliance. The original dataset is archived at ONC. NASA Goddard Space Flight Center, Ocean Ecology Laboratory, Ocean Biology Processing Group provided Moderate-resolution Imaging Spectroradiometer (MODIS) Terra Aqua Chlorophyll Data; NASA OB. DAAC, Greenbelt, MD, USA. https://oceancolor.gsfc.nasa.gov/data/aqua/. Accessed on 06/2016. Victor Smetacek and three anonymous reviewers kindly reviewed the manuscript and discussed the conceptual model of POC export with us. The multi-beam data were provided by Ocean Networks Canada TN282, TN266, TN269, TN254, Ocean Networks Canada/Schmidt Ocean Institute FK009A/B, Canadian Hydrographic Service Tofino Basin 5028091/5027560, J.R. Delaney, D.S. Kelley, and D. Glickson, University of Washington, TN175. | en_US |
| dc.identifier.citation | Davies, T.E.; Maxwell, S.M.; Kaschner, K.; Garilao, C.; & Ban, N.C. (2017). The oceanic biological pump: Rapid carbon transfer to depth at continental margins during winter. Scientific Reports, 7, article 10763. DOI: 10.1038/s41598-017-11075-6 | en_US |
| dc.identifier.uri | https://doi.org/10.1038/s41598-017-11075-6 | |
| dc.identifier.uri | http://hdl.handle.net/1828/10536 | |
| dc.language.iso | en | en_US |
| dc.publisher | Scientific Reports | en_US |
| dc.subject | Ocean Networks Canada | |
| dc.subject.department | Department of Biology | |
| dc.title | The oceanic biological pump: Rapid carbon transfer to depth at continental margins during winter | en_US |
| dc.type | Article | en_US |