Environmental and physiochemical controls on coral calcification along a latitudinal temperature gradient in Western Australia

© 2018 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 25(2019), 2 vom: 19. Feb., Seite 431-447
1. Verfasser: Ross, Claire L (VerfasserIn)
Weitere Verfasser: DeCarlo, Thomas M, McCulloch, Malcolm T
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2019
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Western Australia calcifying fluid carbonate chemistry climate change coral calcification Carbonates
LEADER 01000naa a22002652 4500
001 NLM290884659
003 DE-627
005 20231225065702.0
007 cr uuu---uuuuu
008 231225s2019 xx |||||o 00| ||eng c
024 7 |a 10.1111/gcb.14488  |2 doi 
028 5 2 |a pubmed24n0969.xml 
035 |a (DE-627)NLM290884659 
035 |a (NLM)30456772 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Ross, Claire L  |e verfasserin  |4 aut 
245 1 0 |a Environmental and physiochemical controls on coral calcification along a latitudinal temperature gradient in Western Australia 
264 1 |c 2019 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 18.03.2019 
500 |a Date Revised 26.04.2023 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a © 2018 John Wiley & Sons Ltd. 
520 |a The processes that occur at the micro-scale site of calcification are fundamental to understanding the response of coral growth in a changing world. However, our mechanistic understanding of chemical processes driving calcification is still evolving. Here, we report the results of a long-term in situ study of coral calcification rates, photo-physiology, and calcifying fluid (cf) carbonate chemistry (using boron isotopes, elemental systematics, and Raman spectroscopy) for seven species (four genera) of symbiotic corals growing in their natural environments at tropical, subtropical, and temperate locations in Western Australia (latitudinal range of ~11°). We find that changes in net coral calcification rates are primarily driven by pHcf and carbonate ion concentration [ CO 3 2 - ]cf in conjunction with temperature and DICcf . Coral pHcf varies with latitudinal and seasonal changes in temperature and works together with the seasonally varying DICcf to optimize [ CO 3 2 - ]cf at species-dependent levels. Our results indicate that corals shift their pHcf to adapt and/or acclimatize to their localized thermal regimes. This biological response is likely to have critical implications for predicting the future of coral reefs under CO2 -driven warming and acidification 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Western Australia 
650 4 |a calcifying fluid 
650 4 |a carbonate chemistry 
650 4 |a climate change 
650 4 |a coral calcification 
650 7 |a Carbonates  |2 NLM 
700 1 |a DeCarlo, Thomas M  |e verfasserin  |4 aut 
700 1 |a McCulloch, Malcolm T  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 25(2019), 2 vom: 19. Feb., Seite 431-447  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:25  |g year:2019  |g number:2  |g day:19  |g month:02  |g pages:431-447 
856 4 0 |u http://dx.doi.org/10.1111/gcb.14488  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 25  |j 2019  |e 2  |b 19  |c 02  |h 431-447