{"id":27791,"date":"2021-10-13T12:08:59","date_gmt":"2021-10-13T10:08:59","guid":{"rendered":"https:\/\/www.coralguardian.org\/?p=27791"},"modified":"2021-11-15T12:52:54","modified_gmt":"2021-11-15T11:52:54","slug":"do-corals-store-carbon","status":"publish","type":"post","link":"https:\/\/www.coralguardian.org\/en\/do-corals-store-carbon\/","title":{"rendered":"Do corals store carbon?"},"content":{"rendered":"<p><b>Carbon storage <\/b><span style=\"font-weight: 400;\">in ecosystems is increasingly presented as a way to <\/span><b>fight climate change<\/b><span style=\"font-weight: 400;\">. But the storage and release of carbon by coral skeletons is a complex subject. We will publish several articles in the coming months to explain the debate in detail, starting with this one which is an introduction to the biological <\/span><b>process behind the formation of a coral skeleton.<\/b><\/p>\n<p><span style=\"font-weight: 400;\">The <\/span><b>three-dimensional architecture of coral skeletons<\/b><span style=\"font-weight: 400;\"> allows coral ecosystems to provide habitat, refuge and food for <\/span><b>marine species<\/b><span style=\"font-weight: 400;\">. It also <\/span><b>protects coastlines from erosion<\/b><span style=\"font-weight: 400;\"> by mitigating the force of waves, to the benefit of human communities around the world. Thus, by the very shape of their skeleton, corals are invaluable to the marine ecosystem, but also to coastal communities.<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><b>Coral skeletons\u2019 formation<\/b><\/p>\n<p><span style=\"font-weight: 400;\">Hermatypic corals (also known as <\/span><b>reef-building corals<\/b><span style=\"font-weight: 400;\">) are at the origin of the reefs\u2019 limestone framework, the biomineral structure on which the entire ecosystem rests. Unlike soft corals (Gorgonians, Antipatharians, Alcyonacea corals) whose calcium carbonate skeleton is in the form of calcite, the rigidity of the <\/span><b>aragonite-shape limestone skeleton of reef-building corals<\/b><span style=\"font-weight: 400;\"> makes them perfect reef engineers (Allemand <\/span><i><span style=\"font-weight: 400;\">et al.<\/span><\/i><span style=\"font-weight: 400;\">, 2004).<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">The limestone skeleton is responsible for the various shapes of corals. It also contributes to the spread and absorption of light within corals that live in symbiosis with microalgae (also called <\/span><b>zooxanthellae<\/b><span style=\"font-weight: 400;\">) (Enriquez <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">., 2005). <\/span><b>Calcification<\/b><span style=\"font-weight: 400;\">, or <\/span><b>biomineralization<\/b><span style=\"font-weight: 400;\">, is the rate at which corals produce their skeleton. Through this process, the <\/span><b>calcium carbonate skeleton<\/b> <b>(CaCO<\/b><b>3<\/b><b>)<\/b><span style=\"font-weight: 400;\"> is crystallized in the form of <\/span><b>aragonite<\/b><span style=\"font-weight: 400;\"> (Courtial <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">., 2021). This, thanks to the accumulation and transformation of calcium and carbon.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The carbon can have <\/span><b>two origins<\/b><span style=\"font-weight: 400;\"> : from <\/span><b>carbon dioxide<\/b><span style=\"font-weight: 400;\"> (CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\">) produced with coral respiration, and <\/span><b>bicarbonate ions<\/b><span style=\"font-weight: 400;\"> (HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">&#8211;<\/span><span style=\"font-weight: 400;\">) present in seawater.\u00a0<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Calcium ions (Ca<\/span><span style=\"font-weight: 400;\">2+<\/span><span style=\"font-weight: 400;\">) and bicarbonate ions (HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">&#8211;<\/span><span style=\"font-weight: 400;\">), that are available in seawater, are captured by the coral\u2019s polyps and carried through four layers of cells to reach the <\/span><b>calicoblastic cells<\/b><span style=\"font-weight: 400;\">, which is the last layer before the limestone skeleton (Tambutt\u00e9 <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">., 2011). It is also here that the carbon dioxide is transformed into bicarbonate ions as shown in the following reaction (1) :<\/span><\/li>\n<\/ul>\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\"> + H<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\">O <\/span><span style=\"font-weight: 400;\">\u21d4<\/span><span style=\"font-weight: 400;\"> HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">&#8211;<\/span><span style=\"font-weight: 400;\"> + H<\/span><span style=\"font-weight: 400;\">+<\/span><b> (1)<\/b><span style=\"font-weight: 400;\"><br \/>\n<\/span><span style=\"font-weight: 400;\">Carbon dioxide + water <\/span><span style=\"font-weight: 400;\">\u21d4<\/span><span style=\"font-weight: 400;\"> Bicarbonate ions + hydrogen ions<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Once settled, <\/span><b>bicarbonate and calcium ions are transformed into<\/b> <b>calcium carbonate<\/b><span style=\"font-weight: 400;\">, while, at the same time, a hydrogen ion is released following reaction (2). These hydrogen ions will react with bicarbonate ions <\/span><b>to produce CO<\/b><b>2<\/b><span style=\"font-weight: 400;\">, following reaction (1).<\/span><\/p>\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Ca<\/span><span style=\"font-weight: 400;\">2+<\/span><span style=\"font-weight: 400;\"> + HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">\u2212<\/span><span style=\"font-weight: 400;\"> \u21d4 CaCO<\/span><span style=\"font-weight: 400;\">3 <\/span><span style=\"font-weight: 400;\">+ H<\/span><span style=\"font-weight: 400;\">+<\/span> <b>(2)<\/b><span style=\"font-weight: 400;\"><br \/>\n<\/span><span style=\"font-weight: 400;\"> Calcium ions + Carbonate ions \u21d4 Calcium carbonate + Hydrogen ions<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Finally, <\/span><b>calcium carbonate formation<\/b><span style=\"font-weight: 400;\"> occurs as shown in reaction (3) :<\/span><\/p>\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Ca<\/span><span style=\"font-weight: 400;\">2+<\/span><span style=\"font-weight: 400;\"> + 2 HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">\u2212<\/span><span style=\"font-weight: 400;\">\u21d4<\/span><span style=\"font-weight: 400;\"> CaCO<\/span><span style=\"font-weight: 400;\">3 <\/span><span style=\"font-weight: 400;\">+ CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\"> + H<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\">O <\/span><b>(3)<\/b><span style=\"font-weight: 400;\"><br \/>\n<\/span><span style=\"font-weight: 400;\">Calcium ions + Carbonate ions <\/span><span style=\"font-weight: 400;\">\u21d4<\/span><span style=\"font-weight: 400;\"> Calcium carbonate + Carbon dioxide + water<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">The calcium carbonate (CaCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">) is precipitated in aragonite crystals, <\/span><b>bricks of the coral skeleton<\/b><span style=\"font-weight: 400;\">. In fact, the biomineralization process repeats to form an aragonite chain that constitutes the skeleton. However, it is the <\/span><b>organic matrix<\/b><span style=\"font-weight: 400;\"> that defines the structure of these crystals\u2019 succession imposing a specific morphology to the coral. It is composed of <\/span><b>proteins, lipids and carbohydrates that guide the limestone skeleton formation <\/b><span style=\"font-weight: 400;\">(Reyes-Bermudez <\/span><i><span style=\"font-weight: 400;\">et al.<\/span><\/i><span style=\"font-weight: 400;\">, 2009).\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Therefore, the <\/span><b>skeleton formation<\/b><span style=\"font-weight: 400;\">, or biomineralization, is a process that requires both the transport of <\/span><b>ions to the cells <\/b><span style=\"font-weight: 400;\">and the supervision of the <\/span><b>construction by the coral organic matrix<\/b><span style=\"font-weight: 400;\"> at the same time.<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\" wp-image-27863 aligncenter\" src=\"https:\/\/www.coralguardian.org\/wp-content\/uploads\/2021\/10\/Sche\u0301ma-Biomine\u0301ralisation_VF_AN.png\" alt=\"biomineralisation coral\" width=\"447\" height=\"444\" srcset=\"https:\/\/www.coralguardian.org\/app\/uploads\/2021\/10\/Sche\u0301ma-Biomine\u0301ralisation_VF_AN.png 484w, https:\/\/www.coralguardian.org\/app\/uploads\/2021\/10\/Sche\u0301ma-Biomine\u0301ralisation_VF_AN-300x298.png 300w, https:\/\/www.coralguardian.org\/app\/uploads\/2021\/10\/Sche\u0301ma-Biomine\u0301ralisation_VF_AN-150x150.png 150w, https:\/\/www.coralguardian.org\/app\/uploads\/2021\/10\/Sche\u0301ma-Biomine\u0301ralisation_VF_AN-125x125.png 125w\" sizes=\"(max-width: 447px) 100vw, 447px\" \/><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\"><span style=\"text-decoration: underline;\">Figure 1:<\/span> simplified layout of carbon transport for the coral skeleton\u2019s formation, inside coral layers. Source: self elaboration based on Furla <\/span><i><span style=\"font-weight: 400;\">et al. <\/span><\/i><span style=\"font-weight: 400;\">(2000), Allemand <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">. (2004) and Tambutt\u00e9 <\/span><i><span style=\"font-weight: 400;\">et al. <\/span><\/i><span style=\"font-weight: 400;\">(2011).<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><b>Carbon capture and release by corals<\/b><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">Through biomineralization and photosynthesis by the zooxanthellae, corals are trading platforms that are both <\/span><b>sinks and sources of inorganic carbon<\/b><span style=\"font-weight: 400;\">. Via <\/span><b>photosynthesis<\/b><span style=\"font-weight: 400;\">, symbiotic zooxanthellae present in corals\u2019 tissues consume CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\"> and provide corals with oxygen (Courtial <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">., 2021). Regarding <\/span><b>biomineralization<\/b><span style=\"font-weight: 400;\">, <\/span><b>the coral captures carbon dioxide and bicarbonate ions to build its limestone skeleton.<\/b><\/p>\n<p><span style=\"font-weight: 400;\">However, during calcification, the <\/span><b>hydrogen ions<\/b> <b>(H<\/b><b>+<\/b><b>)<\/b><span style=\"font-weight: 400;\">, produced in the reactions\u00a0 (1) and (2), react with the bicarbonate ions (HCO<\/span><span style=\"font-weight: 400;\">3<\/span><span style=\"font-weight: 400;\">&#8211;<\/span><span style=\"font-weight: 400;\">) to produce CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\">, in the reverse way of reaction (1). This means that the production and liberation of CO<\/span><span style=\"font-weight: 400;\">2<\/span><span style=\"font-weight: 400;\"> is induced in the coral tissue, using the excess of H<\/span><span style=\"font-weight: 400;\">+<\/span><span style=\"font-weight: 400;\"> after the skeleton formation, in order to re-establish the equilibrium (Allemand <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">., 2004). <\/span><b>Biomineralization in corals becomes a source of carbon through the release of CO<\/b><b>2<\/b><b> occurring during the transformation of hydrogen ions. In fact, in the marine environment, for each unit (mol) of CaCO<\/b><b>3<\/b><b> precipitated, 0.6 units (mol) of CO<\/b><b>2<\/b><b> are released<\/b><span style=\"font-weight: 400;\"> (Ware, 1991).\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">On the other hand, <\/span><b>coral respiration<\/b><span style=\"font-weight: 400;\"> releases carbon dioxide. Although some of it is used by zooxanthellae, another part of the carbon ends up in the sea.<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><b>Coral and carbon debate<\/b><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">There is a large <\/span><b>debate around the role of corals in carbon capture<\/b> <b>and release<\/b><span style=\"font-weight: 400;\">, on both an individual scale and on the scale of the whole ecosystem. The scientific community is often confronted with the complexity of the processes related to the different scales, as well as the variations present within reefs in natural environments.<\/span><\/p>\n<p><b>What would be the impact of this inorganic carbon ratio (stored\/released) on the scale of an entire reef?<\/b><span style=\"font-weight: 400;\"> In light of current climate challenges, the storage and release of inorganic carbon within the oceans raises questions about the function of coral reefs in the carbon balance and the threats they face, especially regarding the formation of their skeleton and the support of the ecosystem.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">We will be writing short articles over the next few months to introduce you to this fascinating debate, and to try to shed some light on the subject!<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"text-decoration: underline;\"><span style=\"font-weight: 400;\">Bibliography :<\/span><\/span><\/p>\n<p><span style=\"font-weight: 400;\">Allemand, D., Ferrier-Pag\u00e8s, C., Furla, P., Houlbr\u00e8que, F., Puverel, S., Reynaud, S., Tambutt\u00e9, \u00c9., Tambutt\u00e9, S., &amp; Zoccola, D. (2004). Biomineralisation in reef-building corals: From molecular mechanisms to environmental control. <\/span><i><span style=\"font-weight: 400;\">Comptes Rendus Palevol<\/span><\/i><span style=\"font-weight: 400;\">, <\/span><i><span style=\"font-weight: 400;\">3<\/span><\/i><span style=\"font-weight: 400;\">(6), 453\u2013467. <\/span><a href=\"https:\/\/doi.org\/10.1016\/j.crpv.2004.07.011\"><span style=\"font-weight: 400;\">https:\/\/doi.org\/10.1016\/j.crpv.2004.07.011<\/span><\/a><\/p>\n<p><span style=\"font-weight: 400;\">COURTIAL Lucile &#8211; ALLEMAND Denis &#8211; FURLA Paola (2021), <\/span><i><span style=\"font-weight: 400;\">Coraux : les ing\u00e9nieurs des oc\u00e9ans sont menac\u00e9s<\/span><\/i><span style=\"font-weight: 400;\">, Encyclop\u00e9die de l\u2019Environnement, [en ligne ISSN 2555-0950] url : <\/span><a href=\"http:\/\/www.encyclopedie-environnement.org\/?p=4737\"><span style=\"font-weight: 400;\">http:\/\/www.encyclopedie-environnement.org\/?p=4737<\/span><\/a><\/p>\n<p><span style=\"font-weight: 400;\">Enriquez, S., M\u00e9ndez, E.R., Iglesias-Prieto, R., (2005). Multiple scattering on coral skeletons enhances light absorption by symbiotic algae. Limnol. Oceanogr. 50 (4),1025\u2013103.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Furla, P. <\/span><i><span style=\"font-weight: 400;\">et al<\/span><\/i><span style=\"font-weight: 400;\">. (2000) \u2018Sources and mechanisms of inorganic carbon transport for coral calcification and photosynthesis\u2019, Journal of Experimental Biology, 203(22), pp. 3445\u20133457. doi:10.1242\/jeb.203.22.3445.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Gattuso, J., Pichon, M., Delesalle, B., Canon, C., &amp; Frankignoulle, M. (1996). Carbon fluxes in coral reefs. I. Lagrangian measurement of community metabolism and resulting air-sea CO2 disequilibrium. <\/span><i><span style=\"font-weight: 400;\">Marine Ecology Progress Series<\/span><\/i><span style=\"font-weight: 400;\">, <\/span><i><span style=\"font-weight: 400;\">145<\/span><\/i><span style=\"font-weight: 400;\">, 109\u2013121. <\/span><span style=\"font-weight: 400;\">https:\/\/doi.org\/10.3354\/meps145109<\/span><span style=\"font-weight: 400;\">\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Reyes-Bermudez, A., Lin, Z., Hayward, D.C. et al, (2009). Differential expression of three galaxin-related genes during settlement and metamorphosis in the scleractinian coral Acropora millepora. BMC Evol Biol 9, 178. https:\/\/doi.org\/10.1186\/1471-2148-9-178<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Tambutt\u00e9, S., Holcomb, M., Ferrier-Pag\u00e8s, C., Reynaud, S., Tambutt\u00e9, \u00c9., Zoccola, D., &amp; Allemand, D. (2011). Coral biomineralization: From the gene to the environment. <\/span><i><span style=\"font-weight: 400;\">Journal of Experimental Marine Biology and Ecology<\/span><\/i><span style=\"font-weight: 400;\">, <\/span><i><span style=\"font-weight: 400;\">408<\/span><\/i><span style=\"font-weight: 400;\">(1), 58\u201378. <\/span><a href=\"https:\/\/doi.org\/10.1016\/j.jembe.2011.07.026\"><span style=\"font-weight: 400;\">https:\/\/doi.org\/10.1016\/j.jembe.2011.07.026<\/span><\/a><\/p>\n<p><span style=\"font-weight: 400;\">Ware, J.R., 1991. Coral reefs: sources or sinks of atmospheric CO2? <\/span><i><span style=\"font-weight: 400;\">Coral Reefs<\/span><\/i><span style=\"font-weight: 400;\"> 11, 127\u2013130. <\/span><a href=\"https:\/\/doi.org\/10.1007\/BF00255465\"><span style=\"font-weight: 400;\">h<\/span><span style=\"font-weight: 400;\">ttps:\/\/doi.org\/10.1007\/BF00255465<\/span><\/a><\/p>\n<div role=\"form\" class=\"wpcf7\" id=\"wpcf7-f22507-p22507-o1\" lang=\"en-US\" dir=\"ltr\"><div><div class=\"wpcf7-form\"><div class=\"fit-the-fullspace\"><div><div class=\"screen-reader-response\"><p role=\"status\" aria-live=\"polite\" aria-atomic=\"true\"><\/p> <ul><\/ul><\/div><form action=\"\/en\/wp-json\/wp\/v2\/posts\/27791#wpcf7-f22507-p22507-o1\" method=\"post\" class=\"wpcf7-form init\" enctype=\"\" autocomplete=\"autocomplete\" novalidate=\"novalidate\" data-status=\"init\" locale=\"en_US\"><div style=\"display: block;\"><input type=\"hidden\" name=\"_wpcf7\" value=\"22507\" \/>\n<input type=\"hidden\" name=\"_wpcf7_version\" value=\"5.8.6\" \/>\n<input type=\"hidden\" name=\"_wpcf7_locale\" value=\"en_US\" \/>\n<input type=\"hidden\" name=\"_wpcf7_unit_tag\" value=\"wpcf7-f22507-p22507-o1\" \/>\n<input type=\"hidden\" name=\"_wpcf7_posted_data_hash\" value=\"\" \/>\n<input type=\"hidden\" name=\"_wpcf7_fit-the-fullspace\" value=\"\" \/>\n<\/div><p><label> Your name<br \/>\n<span class=\"wpcf7-form-control-wrap\" data-name=\"your-name\"><input size=\"40\" class=\"wpcf7-form-control wpcf7-text wpcf7-validates-as-required\" autocomplete=\"name\" aria-required=\"true\" aria-invalid=\"false\" value=\"\" type=\"text\" name=\"your-name\" \/><\/span> <\/label>\n<\/p>\n<p><label> Your email<br \/>\n<span class=\"wpcf7-form-control-wrap\" data-name=\"your-email\"><input size=\"40\" class=\"wpcf7-form-control wpcf7-email wpcf7-validates-as-required wpcf7-text wpcf7-validates-as-email\" autocomplete=\"email\" aria-required=\"true\" aria-invalid=\"false\" value=\"\" type=\"email\" name=\"your-email\" \/><\/span> <\/label>\n<\/p>\n<p><label> Subject<br \/>\n<span class=\"wpcf7-form-control-wrap\" data-name=\"your-subject\"><input size=\"40\" class=\"wpcf7-form-control wpcf7-text wpcf7-validates-as-required\" aria-required=\"true\" aria-invalid=\"false\" value=\"\" type=\"text\" name=\"your-subject\" \/><\/span> <\/label>\n<\/p>\n<p><label> Your message (optional)<br \/>\n<span class=\"wpcf7-form-control-wrap\" data-name=\"your-message\"><textarea cols=\"40\" rows=\"10\" class=\"wpcf7-form-control wpcf7-textarea\" aria-invalid=\"false\" name=\"your-message\"><\/textarea><\/span> <\/label>\n<\/p>\n<p><input class=\"wpcf7-form-control wpcf7-submit has-spinner\" type=\"submit\" value=\"Submit\" \/>\n<\/p><div class=\"wpcf7-response-output\" aria-hidden=\"true\"><\/div><\/form><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Carbon storage in ecosystems is increasingly presented as a way to fight climate change. But the storage and release of carbon by coral skeletons is&#8230; <\/p>\n","protected":false},"author":15,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[12],"tags":[600],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v21.8 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Do corals store or release carbon? | Article by Coral Guardian<\/title>\n<meta name=\"description\" content=\"Discover the non-profit Coral Guardian&#039;s article on the storage and release of carbon within coral reefs. 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