210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef

Here we show the use of the 210 Pb- 226 Ra excess method to determine the growth rate of two corals from the world's largest known cold-water coral reef, Røst Reef, north of the Arctic circle off Norway. Colonies of each of the two species that build the reef, Lophelia pertusa and Madrepora ocu...

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Published in:Biogeosciences
Main Authors: N. Tisnérat-Laborde, L. Bordier, N. Frank, C. Colin, J. M. Hall-Spencer, J.-L. Reyss, P. Sabatier, E. Douville
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2012
Subjects:
Online Access:https://doi.org/10.5194/bg-9-1253-2012
https://doaj.org/article/ddec422ec3824f82a1fd5d8db6c66e72
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spelling ftdoajarticles:oai:doaj.org/article:ddec422ec3824f82a1fd5d8db6c66e72 2023-05-15T15:19:04+02:00 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef N. Tisnérat-Laborde L. Bordier N. Frank C. Colin J. M. Hall-Spencer J.-L. Reyss P. Sabatier E. Douville 2012-03-01T00:00:00Z https://doi.org/10.5194/bg-9-1253-2012 https://doaj.org/article/ddec422ec3824f82a1fd5d8db6c66e72 EN eng Copernicus Publications http://www.biogeosciences.net/9/1253/2012/bg-9-1253-2012.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-9-1253-2012 1726-4170 1726-4189 https://doaj.org/article/ddec422ec3824f82a1fd5d8db6c66e72 Biogeosciences, Vol 9, Iss 3, Pp 1253-1265 (2012) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2012 ftdoajarticles https://doi.org/10.5194/bg-9-1253-2012 2022-12-30T22:28:46Z Here we show the use of the 210 Pb- 226 Ra excess method to determine the growth rate of two corals from the world's largest known cold-water coral reef, Røst Reef, north of the Arctic circle off Norway. Colonies of each of the two species that build the reef, Lophelia pertusa and Madrepora oculata , were collected alive at 350 m depth using a submersible. Pb and Ra isotopes were measured along the major growth axis of both specimens using low level alpha and gamma spectrometry and trace element compositions were studied. 210 Pb and 226 Ra differ in the way they are incorporated into coral skeletons. Hence, to assess growth rates, we considered the exponential decrease of initially incorporated 210 Pb, as well as the increase in 210 Pb from the decay of 226 Ra and contamination with 210 Pb associated with Mn-Fe coatings that we were unable to remove completely from the oldest parts of the skeletons. 226 Ra activity was similar in both coral species, so, assuming constant uptake of 210 Pb through time, we used the 210 Pb- 226 Ra chronology to calculate growth rates. The 45.5 cm long branch of M. oculata was 31 yr with an average linear growth rate of 14.4 ± 1.1 mm yr −1 (2.6 polyps per year). Despite cleaning, a correction for Mn-Fe oxide contamination was required for the oldest part of the colony; this correction corroborated our radiocarbon date of 40 yr and a mean growth rate of 2 polyps yr −1 . This rate is similar to the one obtained in aquarium experiments under optimal growth conditions. For the 80 cm-long L. pertusa colony, metal-oxide contamination remained in both the middle and basal part of the coral skeleton despite cleaning, inhibiting similar age and growth rate estimates. The youngest part of the colony was free of metal oxides and this 15 cm section had an estimated a growth rate of 8 mm yr −1 , with high uncertainty (~1 polyp every two to three years). We are less certain of this 210 Pb growth rate estimate which is within the lowermost ranges of previous growth rate estimates. We show that 210 ... Article in Journal/Newspaper Arctic Lophelia pertusa Directory of Open Access Journals: DOAJ Articles Arctic Norway Røst ENVELOPE(11.983,11.983,67.467,67.467) Biogeosciences 9 3 1253 1265
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
N. Tisnérat-Laborde
L. Bordier
N. Frank
C. Colin
J. M. Hall-Spencer
J.-L. Reyss
P. Sabatier
E. Douville
210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
description Here we show the use of the 210 Pb- 226 Ra excess method to determine the growth rate of two corals from the world's largest known cold-water coral reef, Røst Reef, north of the Arctic circle off Norway. Colonies of each of the two species that build the reef, Lophelia pertusa and Madrepora oculata , were collected alive at 350 m depth using a submersible. Pb and Ra isotopes were measured along the major growth axis of both specimens using low level alpha and gamma spectrometry and trace element compositions were studied. 210 Pb and 226 Ra differ in the way they are incorporated into coral skeletons. Hence, to assess growth rates, we considered the exponential decrease of initially incorporated 210 Pb, as well as the increase in 210 Pb from the decay of 226 Ra and contamination with 210 Pb associated with Mn-Fe coatings that we were unable to remove completely from the oldest parts of the skeletons. 226 Ra activity was similar in both coral species, so, assuming constant uptake of 210 Pb through time, we used the 210 Pb- 226 Ra chronology to calculate growth rates. The 45.5 cm long branch of M. oculata was 31 yr with an average linear growth rate of 14.4 ± 1.1 mm yr −1 (2.6 polyps per year). Despite cleaning, a correction for Mn-Fe oxide contamination was required for the oldest part of the colony; this correction corroborated our radiocarbon date of 40 yr and a mean growth rate of 2 polyps yr −1 . This rate is similar to the one obtained in aquarium experiments under optimal growth conditions. For the 80 cm-long L. pertusa colony, metal-oxide contamination remained in both the middle and basal part of the coral skeleton despite cleaning, inhibiting similar age and growth rate estimates. The youngest part of the colony was free of metal oxides and this 15 cm section had an estimated a growth rate of 8 mm yr −1 , with high uncertainty (~1 polyp every two to three years). We are less certain of this 210 Pb growth rate estimate which is within the lowermost ranges of previous growth rate estimates. We show that 210 ...
format Article in Journal/Newspaper
author N. Tisnérat-Laborde
L. Bordier
N. Frank
C. Colin
J. M. Hall-Spencer
J.-L. Reyss
P. Sabatier
E. Douville
author_facet N. Tisnérat-Laborde
L. Bordier
N. Frank
C. Colin
J. M. Hall-Spencer
J.-L. Reyss
P. Sabatier
E. Douville
author_sort N. Tisnérat-Laborde
title 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
title_short 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
title_full 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
title_fullStr 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
title_full_unstemmed 210 Pb- 226 Ra chronology reveals rapid growth rate of Madrepora oculata and Lophelia pertusa on world's largest cold-water coral reef
title_sort 210 pb- 226 ra chronology reveals rapid growth rate of madrepora oculata and lophelia pertusa on world's largest cold-water coral reef
publisher Copernicus Publications
publishDate 2012
url https://doi.org/10.5194/bg-9-1253-2012
https://doaj.org/article/ddec422ec3824f82a1fd5d8db6c66e72
long_lat ENVELOPE(11.983,11.983,67.467,67.467)
geographic Arctic
Norway
Røst
geographic_facet Arctic
Norway
Røst
genre Arctic
Lophelia pertusa
genre_facet Arctic
Lophelia pertusa
op_source Biogeosciences, Vol 9, Iss 3, Pp 1253-1265 (2012)
op_relation http://www.biogeosciences.net/9/1253/2012/bg-9-1253-2012.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
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1726-4170
1726-4189
https://doaj.org/article/ddec422ec3824f82a1fd5d8db6c66e72
op_doi https://doi.org/10.5194/bg-9-1253-2012
container_title Biogeosciences
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