Show simple item record

dc.contributor.authorLovecchio, E
dc.contributor.authorLenton, TM
dc.date.accessioned2020-06-04T15:16:40Z
dc.date.issued2020-04-09
dc.description.abstractThe biological pump of the ocean has changed over Earth's history, from one dominated by prokaryotes to one involving a mixture of prokaryotes and eukaryotes with trophic structure. Changes in the biological pump are in turn hypothesized to have caused important changes in the nutrient and redox properties of the ocean. To explore these hypotheses, we present here a new box model including oxygen (O), phosphorus (P) and a dynamical biological pump. Our Biological Pump, Oxygen and Phosphorus (BPOP) model accounts for two – small and large – organic matter species generated by production and coagulation, respectively. Export and burial of these particles are regulated by a remineralization length (zrem) scheme. We independently vary zrem of small and large particles in order to study how changes in sinking speeds and remineralization rates affect the major biogeochemical fluxes and O and P ocean concentrations. Modeled O and P budgets and fluxes lie reasonably close to present estimates for zrem in the range of currently measured values. Our results highlight that relatively small changes in zrem of the large particles can have important impacts on the O and P ocean availability and support the idea that an early ocean dominated by small particles was nutrient rich due to the inefficient removal of P to sediments. The results also suggest that extremely low oxygen concentrations in the shelf can coexist with an oxygenated deep open ocean for realistic values of zrem, especially for large values of the small-particle zrem. This could challenge conventional interpretations that the Proterozoic deep ocean was anoxic, which are derived from shelf and slope sediment redox data. This simple and computationally inexpensive model is a promising tool to investigate the impact of changes in the organic matter sinking and remineralization rates as well as changes in physical processes coupled with the biological pump in a variety of case studies.en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.identifier.citationVol. 13, pp. 1865 - 1883en_GB
dc.identifier.doi10.5194/gmd-13-1865-2020
dc.identifier.grantnumberNE/P013651/1en_GB
dc.identifier.urihttp://hdl.handle.net/10871/121280
dc.language.isoenen_GB
dc.publisherEuropean Geosciences Union (EGU)en_GB
dc.rights© Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.en_GB
dc.titleBPOP-v1 model: exploring the impact of changes in the biological pump on the shelf sea and ocean nutrient and redox stateen_GB
dc.typeArticleen_GB
dc.date.available2020-06-04T15:16:40Z
dc.identifier.issn1991-959X
dc.descriptionThis is the final version. Available from the publisher via the DOI in this record.en_GB
dc.identifier.journalGeoscientific Model Developmenten_GB
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2020-02-25
exeter.funder::Natural Environment Research Council (NERC)en_GB
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2020-04-09
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2020-06-04T14:40:07Z
refterms.versionFCDVoR
refterms.dateFOA2020-06-04T15:16:45Z
refterms.panelCen_GB
refterms.depositExceptionpublishedGoldOA
refterms.depositExceptionExplanationhttps://doi.org/10.5194/gmd-13-1865-2020


Files in this item

This item appears in the following Collection(s)

Show simple item record

© Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.
Except where otherwise noted, this item's licence is described as © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.