Coral reef development in response to large amplitude internal waves and monsoon impact ...

The Andaman Sea and other macrotidal semi-enclosed tropical seas feature large amplitude internal waves (LAIW). Although LAIW induce strong fluctuations i.e. of temperature, pH, and nutrients, their influence on reef development is so far unknown. A better-known source of disturbance is the monsoon...

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Main Authors: Wall, Marlene, Schmidt, Gertraud, Janjang, Pornpang, Khokiattiwong, Somkiat, Richter, Claudio
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.831254
https://doi.pangaea.de/10.1594/PANGAEA.831254
id ftdatacite:10.1594/pangaea.831254
record_format openpolar
spelling ftdatacite:10.1594/pangaea.831254 2024-09-15T18:28:14+00:00 Coral reef development in response to large amplitude internal waves and monsoon impact ... Wall, Marlene Schmidt, Gertraud Janjang, Pornpang Khokiattiwong, Somkiat Richter, Claudio 2012 application/zip https://dx.doi.org/10.1594/pangaea.831254 https://doi.pangaea.de/10.1594/PANGAEA.831254 en eng PANGAEA https://dx.doi.org/10.1371/journal.pone.0050207 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Biological Impacts of Ocean Acidification BIOACID article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.83125410.1371/journal.pone.0050207 2024-08-01T10:54:59Z The Andaman Sea and other macrotidal semi-enclosed tropical seas feature large amplitude internal waves (LAIW). Although LAIW induce strong fluctuations i.e. of temperature, pH, and nutrients, their influence on reef development is so far unknown. A better-known source of disturbance is the monsoon affecting corals due to turbulent mixing and sedimentation. Because in the Andaman Sea both, LAIW and monsoon, act from the same westerly direction their relative contribution to reef development is difficult to discern. Here, we explore the framework development in a number of offshore island locations subjected to differential LAIW- and SW-monsoon impact to address this open question. Cumulative negative temperature anomalies - a proxy for LAIW impact - explained a higher percentage of the variability in coral reef framework height, than sedimentation rates which resulted mainly from the monsoon. Temperature anomalies and sediment grain size provided the best correlation with framework height suggesting that so ... : CalMarO - Calcification by marine organisms, PEOPLE-2007-1-1-ITN Marie Curie Action: 215157BioAcid - German Ministry for Education and Research Project (Bmbf), Grant number 03F0608B, Bioacid 3.2.3, Coral Calcification in marginal reefsORCAS - Ocean Reef Coupling in the Andaman Sea - German Research Foundation (DFG), Grant number RI 1074/7-1 ... Article in Journal/Newspaper Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Biological Impacts of Ocean Acidification BIOACID
spellingShingle Biological Impacts of Ocean Acidification BIOACID
Wall, Marlene
Schmidt, Gertraud
Janjang, Pornpang
Khokiattiwong, Somkiat
Richter, Claudio
Coral reef development in response to large amplitude internal waves and monsoon impact ...
topic_facet Biological Impacts of Ocean Acidification BIOACID
description The Andaman Sea and other macrotidal semi-enclosed tropical seas feature large amplitude internal waves (LAIW). Although LAIW induce strong fluctuations i.e. of temperature, pH, and nutrients, their influence on reef development is so far unknown. A better-known source of disturbance is the monsoon affecting corals due to turbulent mixing and sedimentation. Because in the Andaman Sea both, LAIW and monsoon, act from the same westerly direction their relative contribution to reef development is difficult to discern. Here, we explore the framework development in a number of offshore island locations subjected to differential LAIW- and SW-monsoon impact to address this open question. Cumulative negative temperature anomalies - a proxy for LAIW impact - explained a higher percentage of the variability in coral reef framework height, than sedimentation rates which resulted mainly from the monsoon. Temperature anomalies and sediment grain size provided the best correlation with framework height suggesting that so ... : CalMarO - Calcification by marine organisms, PEOPLE-2007-1-1-ITN Marie Curie Action: 215157BioAcid - German Ministry for Education and Research Project (Bmbf), Grant number 03F0608B, Bioacid 3.2.3, Coral Calcification in marginal reefsORCAS - Ocean Reef Coupling in the Andaman Sea - German Research Foundation (DFG), Grant number RI 1074/7-1 ...
format Article in Journal/Newspaper
author Wall, Marlene
Schmidt, Gertraud
Janjang, Pornpang
Khokiattiwong, Somkiat
Richter, Claudio
author_facet Wall, Marlene
Schmidt, Gertraud
Janjang, Pornpang
Khokiattiwong, Somkiat
Richter, Claudio
author_sort Wall, Marlene
title Coral reef development in response to large amplitude internal waves and monsoon impact ...
title_short Coral reef development in response to large amplitude internal waves and monsoon impact ...
title_full Coral reef development in response to large amplitude internal waves and monsoon impact ...
title_fullStr Coral reef development in response to large amplitude internal waves and monsoon impact ...
title_full_unstemmed Coral reef development in response to large amplitude internal waves and monsoon impact ...
title_sort coral reef development in response to large amplitude internal waves and monsoon impact ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.831254
https://doi.pangaea.de/10.1594/PANGAEA.831254
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.1371/journal.pone.0050207
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83125410.1371/journal.pone.0050207
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