Iron defecation by sperm whales stimulates carbon export in the Southern Ocean

The iron-limited Southern Ocean plays an important role in regulating atmospheric CO2 levels. Marine mammal respiration has been proposed to decrease the efficiency of the Southern Ocean biological pump by returning photosynthetically fixed carbon to the atmosphere. Here, we show that by consuming p...

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Main Authors: Lavery, TJ, Roudnew, B, Gill, P, Seymour, J, Seuront, L, Johnson, G, Mitchell, JG, Smetacek, V
Format: Article in Journal/Newspaper
Language:unknown
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/10453/13378
id ftunivtsydney:oai:opus.lib.uts.edu.au:10453/13378
record_format openpolar
spelling ftunivtsydney:oai:opus.lib.uts.edu.au:10453/13378 2023-05-15T17:59:26+02:00 Iron defecation by sperm whales stimulates carbon export in the Southern Ocean Lavery, TJ Roudnew, B Gill, P Seymour, J Seuront, L Johnson, G Mitchell, JG Smetacek, V 2010-11-22 application/pdf http://hdl.handle.net/10453/13378 unknown Proceedings of the Royal Society B: Biological Sciences 10.1098/rspb.2010.0863 Proceedings of the Royal Society B: Biological Sciences, 2010, 277 (1699), pp. 3527 - 3531 0962-8452 http://hdl.handle.net/10453/13378 Feces Animals Carbon Dioxide Carbon Iron Population Dynamics Oxygen Consumption Defecation Oceans and Seas Sperm Whale Journal Article 2010 ftunivtsydney 2022-03-13T13:34:48Z The iron-limited Southern Ocean plays an important role in regulating atmospheric CO2 levels. Marine mammal respiration has been proposed to decrease the efficiency of the Southern Ocean biological pump by returning photosynthetically fixed carbon to the atmosphere. Here, we show that by consuming prey at depth and defecating iron-rich liquid faeces into the photic zone, sperm whales (Physeter macrocephalus) instead stimulate new primary production and carbon export to the deep ocean. We estimate that Southern Ocean sperm whales defecate 50 tonnes of iron into the photic zone each year. Molar ratios of Cexport : Feadded determined during natural ocean fertilization events are used to estimate the amount of carbon exported to the deep ocean in response to the iron defecated by sperm whales. We find that Southern Ocean sperm whales stimulate the export of 4 × 105 tonnes of carbon per year to the deep ocean and respire only 2 × 10 5 tonnes of carbon per year. By enhancing new primary production, the populations of 12 000 sperm whales in the Southern Ocean act as a carbon sink, removing 2 × 105 tonnes more carbon from the atmosphere than they add during respiration. The ability of the Southern Ocean to act as a carbon sink may have been diminished by large-scale removal of sperm whales during industrial whaling. © 2010 The Royal Society. Article in Journal/Newspaper Physeter macrocephalus Southern Ocean Sperm whale University of Technology Sydney: OPUS - Open Publications of UTS Scholars Southern Ocean
institution Open Polar
collection University of Technology Sydney: OPUS - Open Publications of UTS Scholars
op_collection_id ftunivtsydney
language unknown
topic Feces
Animals
Carbon Dioxide
Carbon
Iron
Population Dynamics
Oxygen Consumption
Defecation
Oceans and Seas
Sperm Whale
spellingShingle Feces
Animals
Carbon Dioxide
Carbon
Iron
Population Dynamics
Oxygen Consumption
Defecation
Oceans and Seas
Sperm Whale
Lavery, TJ
Roudnew, B
Gill, P
Seymour, J
Seuront, L
Johnson, G
Mitchell, JG
Smetacek, V
Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
topic_facet Feces
Animals
Carbon Dioxide
Carbon
Iron
Population Dynamics
Oxygen Consumption
Defecation
Oceans and Seas
Sperm Whale
description The iron-limited Southern Ocean plays an important role in regulating atmospheric CO2 levels. Marine mammal respiration has been proposed to decrease the efficiency of the Southern Ocean biological pump by returning photosynthetically fixed carbon to the atmosphere. Here, we show that by consuming prey at depth and defecating iron-rich liquid faeces into the photic zone, sperm whales (Physeter macrocephalus) instead stimulate new primary production and carbon export to the deep ocean. We estimate that Southern Ocean sperm whales defecate 50 tonnes of iron into the photic zone each year. Molar ratios of Cexport : Feadded determined during natural ocean fertilization events are used to estimate the amount of carbon exported to the deep ocean in response to the iron defecated by sperm whales. We find that Southern Ocean sperm whales stimulate the export of 4 × 105 tonnes of carbon per year to the deep ocean and respire only 2 × 10 5 tonnes of carbon per year. By enhancing new primary production, the populations of 12 000 sperm whales in the Southern Ocean act as a carbon sink, removing 2 × 105 tonnes more carbon from the atmosphere than they add during respiration. The ability of the Southern Ocean to act as a carbon sink may have been diminished by large-scale removal of sperm whales during industrial whaling. © 2010 The Royal Society.
format Article in Journal/Newspaper
author Lavery, TJ
Roudnew, B
Gill, P
Seymour, J
Seuront, L
Johnson, G
Mitchell, JG
Smetacek, V
author_facet Lavery, TJ
Roudnew, B
Gill, P
Seymour, J
Seuront, L
Johnson, G
Mitchell, JG
Smetacek, V
author_sort Lavery, TJ
title Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
title_short Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
title_full Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
title_fullStr Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
title_full_unstemmed Iron defecation by sperm whales stimulates carbon export in the Southern Ocean
title_sort iron defecation by sperm whales stimulates carbon export in the southern ocean
publishDate 2010
url http://hdl.handle.net/10453/13378
geographic Southern Ocean
geographic_facet Southern Ocean
genre Physeter macrocephalus
Southern Ocean
Sperm whale
genre_facet Physeter macrocephalus
Southern Ocean
Sperm whale
op_relation Proceedings of the Royal Society B: Biological Sciences
10.1098/rspb.2010.0863
Proceedings of the Royal Society B: Biological Sciences, 2010, 277 (1699), pp. 3527 - 3531
0962-8452
http://hdl.handle.net/10453/13378
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