{"id":32180,"date":"2023-08-10T08:50:23","date_gmt":"2023-08-10T06:50:23","guid":{"rendered":"https:\/\/www.coralguardian.org\/un-benefice-inattendu-pour-certains-coraux-au-pacifique-de-el-nino\/"},"modified":"2023-08-10T09:07:10","modified_gmt":"2023-08-10T07:07:10","slug":"an-unexpected-benefit-for-some-pacific-corals-of-el-nino","status":"publish","type":"post","link":"https:\/\/www.coralguardian.org\/en\/an-unexpected-benefit-for-some-pacific-corals-of-el-nino\/","title":{"rendered":"An unexpected benefit for some Pacific corals of El Ni\u00f1o?"},"content":{"rendered":"

Over the past 30 years, <\/span>marine heat waves<\/b> have become increasingly frequent, intense and long, and it’s highly likely that this trend will increase with global warming (Fr\u00f6licher, 2018).<\/span><\/p>\n

What are marine heat waves<\/b>? The precise definition of these events can vary from one study to another, but scientists agree that they are episodes lasting at least five days (and up to several months) when the sea surface temperatures are above the historical average (at least 30 years data) (Hobday<\/span> et al<\/span><\/i>., 2016; Viglione, 2021). They can occur as a result of complex oceanic or atmospheric dynamics, such as the El Ni\u00f1o phenomenon (Claar <\/span>et al<\/span><\/i>., 2018).<\/span><\/p>\n

El Ni\u00f1o is a natural climatic event <\/b>involving a reversal of ocean currents in the Pacific. This results in a rise in temperatures along the South American coast and a change in temperatures across the globe. This event occurs approximately every 2 to 7 years, although <\/span>more extreme events have been reported in the last decades <\/b>(Cai <\/span>et al.<\/span><\/i>, 2014). The consequences of El Ni\u00f1o are far-reaching, both in socio-economic terms, with a heavy impact on fishing activities, and in environmental terms, with diverse effects on marine and terrestrial ecosystems. In coral reef areas, marine heat waves during this phenomenon\u00a0 lead to successive and widespread mass bleaching events, especially the one reported in 2015-2016 with unprecedented thermal stress (Claar <\/span>et al.<\/span><\/i>, 2018 ; Fox <\/span>et al.<\/span><\/i>, 2023).<\/span><\/p>\n

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An international team of researchers led by Dr. Michael Fox from KAUST University wanted to <\/span>investigate the local repercussions of heat waves on local ocean processes, and how this impacts corals\u2019 trophic ecology (what they eat)<\/b>. To do this, they focused on coral reefs at Palmyra Atoll in the Pacific Ocean, before and after the El Ni\u00f1o phenomenon in 2015-2016. Their research showed unexpected results: oceanographic changes during El Ni\u00f1o allowed corals in this location to have <\/span>access to supplementary nutritional sources during heat waves<\/b>, unveiling a new mechanism that operates in corals’ favor (Fox <\/span>et al.<\/span><\/i>, 2023). How does it work? Here, we explain some of the results of their research.<\/span><\/p>\n

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The oceanographic aspect: what happens with El Nino?<\/b><\/p>\n

For their study, Fox’s team described the <\/span>local oceanic repercussions of El Ni\u00f1o in Palmyra Atoll <\/b>(Central Pacific), and then made the link with corals. They observed oceanographic dynamics using 2 distinct variables: the<\/span> speed of the North Equatorial Counter Current<\/b> (*see glossary below) and the depth of the <\/span>oceanic mixing layer<\/b> (*see glossary below).<\/span><\/p>\n

They observed anomalies in both of these parameters during the 2015 El Ni\u00f1o (shaded area in Fig. 1), reflecting an <\/span>upwelling of deep, cold, nutrient-rich water to the surface<\/b>. Indeed, the depth of the mixing layer has never been so shallow (around 15 m, compared with an average depth of 90 m, higher panel, Fig. 1), and current velocity has reached 0.6 m\/s, compared with an average of 0.3 m\/s the rest of the time (lower panel, Fig. 1).<\/span><\/p>\n

First finding: in Palmyra Atoll, during the 2015 El Nino phenomenon, a local upwelling of cool, nutrient-rich water was reported (Fox <\/b>et al.<\/i><\/b>, 2023).<\/b><\/p>\n

This was not the case on all the islands in the region: in other localities, oceanographic parameters do not point towards the occurrence of upwelling (Fig. 2), and indeed coral mortality in these areas was higher than in Palmyra, demonstrating the complexity of the climatic phenomenon (Fox <\/span>et al<\/span><\/i>. 2023).<\/span><\/p>\n

\"graphique\"<\/p>\n

Figure 1: <\/span><\/i>Graph showing the thinning of the surface layer (top) to the increase in North Equatorial Counter Current velocity (bottom) during the 2015 El Ni\u00f1o. Taken and adapted from Fox <\/span>et al<\/span><\/i>., 2023.<\/span><\/h5>\n

\"figure\"<\/p>\n

Figure 2<\/span><\/i>: Graph showing the regional variation of the mixed layer depth anomaly in the Pacific between August and November 2015, compared with the period 1980-2020. Colors: towards brown, the mixed layer is deeper than usual, and towards blue, the layer is shallower than usual. Taken and adapted from Fox <\/span>et al<\/span><\/i>., 2023.<\/span><\/h5>\n

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How do corals respond?<\/b><\/p>\n

Scientists wanted to know how coral food sources varied with upwelling in Palmyra Atoll.<\/span><\/p>\n

Therefore, they studied the trophic ecology of a species of hard coral <\/span>(Pocillopora meandrina<\/span><\/i>) before and after El Ni\u00f1o phenomenon of 2015-2016. This coral species, like most tropical corals, is <\/span>mixotrophic<\/b>, <\/span>meaning<\/b> it has 2 feeding sources<\/b>. Corals receive nutrients through photosynthesis by their microalgae (<\/span>autotrophy<\/b>), and can hunt for food in their environment (<\/span>heterotrophy<\/b>). The choice of food source can vary according to the availability of resources in the environment.<\/span><\/p>\n

In the study, researchers observed a <\/span>shift to heterotrophy in corals during El Ni\u00f1o in 2015 (Fig. 3)<\/b>. This shift cannot be explained by the loss of symbiosis with the microalgae, as no coral bleaching was observed. <\/span>This dietary change can therefore be explained by an increase in the presence of nutrients available to coral during El Ni\u00f1o, coming from the described upwelling.<\/b><\/p>\n

Second result: deep waters brought to the surface by upwelling will provide corals with a new source of food, supplementary to autotrophy-derived nutrients. This phenomenon will favor corals that have a flexible trophic strategy and can transition to heterotrophy, which is an additional nutritional input for corals.<\/b><\/p>\n

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\"figure<\/p>\n

Figure 3: <\/span><\/i>Graph showing transitions to heterotrophy during the El Ni\u00f1o events of 2012, 2014 and 2015.<\/span> Taken and adapted from Fox <\/span>et al.<\/span><\/i>, 2023.<\/span><\/h5>\n

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On top of this, upwelling is associated with<\/span> brief, intense pulses of cold water<\/b>. These would have a cooling effect on waters below 15 m in depth, which increases with depth. Although our understanding of the impact of these “cold pulses” on coral cooling remains limited, the hypothesis that upwelling provides corals with a thermal refuge during El Ni\u00f1o is not ruled out.<\/span><\/p>\n

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In conclusion, the research suggests that these two local oceanographic mechanisms described at Palmyra Atoll during El Ni\u00f1o, <\/span>nutrient supply and thermal refuge,<\/b> contribute to limit the thermal stress and coral bleaching, which would make them more resilient to the extreme conditions to which they are exposed, in the face of climate change. Nevertheless, the El Ni\u00f1o phenomenon remains a very complex event from a global point of view, and with huge impacts on coral reefs. Understanding its effects on a local or regional scale to better predict the vulnerability of reefs to climate change remains fundamental.<\/span><\/p>\n

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Glossary<\/b>:\u00a0<\/span><\/p>\n

The North Equatorial Counter Current<\/b>: is a current that flows from west to east at about 3-10\u00b0N in the Atlantic, Indian Ocean and Pacific basins.<\/span><\/p>\n

The oceanic mixed layer<\/b>: this is the most superficial layer of the ocean in which the water is homogeneous in terms of salinity, temperature, and density. It interacts directly with the atmosphere.<\/span><\/p>\n

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Cited articles:<\/b><\/p>\n

Cai W, Borlace S, Lengaigne M <\/span>et al.<\/span><\/i>(<\/span>2014)<\/span> Increasing frequency of extreme El Ni\u00f1o events due to greenhouse warming. <\/span>Nature<\/span><\/i> Clim Change<\/span><\/i> 4, 111\u2013116. https:\/\/doi.org\/10.1038\/nclimate2100<\/span><\/h5>\n
Claar DC, Szostek L, McDevitt-Irwin JM, Schanze JJ, Baum JK (2018) Global patterns and impacts of El Ni\u00f1o events on coral reefs: A meta-analysis. PLoS ONE 13(2): e0190957. <\/span>https:\/\/doi.org\/10.1371\/journal.pone.0190957<\/span><\/a><\/h5>\n
Fox MD, Guillaume-Castel R, Edwards CB, Glanz J, Gove JM, Green JAM, Juhlin E, Smith JE, Williams GJ. (2023) Ocean currents magnify upwelling and deliver nutritional subsidies to reef-building corals during El Ni\u00f1o heatwaves. Sci Adv. 9(24):eadd5032. doi: 10.1126\/sciadv.add5032. Epub 2023 Jun 14. PMID: 37315146; PMCID: PMC10266739.<\/b><\/h5>\n
Fr\u00f6licher TL, Fischer EM & Gruber N (2018) Marine heatwaves under global warming. <\/span>Nature<\/span><\/i> 560, 360\u2013364. <\/span>https:\/\/doi.org\/10.1038\/s41586-018-0383-9<\/span><\/a><\/h5>\n
Hobday AJ, Alexander LV, Perkins SE, Smale DA, Straub SC, et al. (2016). A hierarchical approach to defining marine heatwaves. <\/span>Prog. Oceanogr.<\/span><\/i> 141:227\u201338 <\/span>https:\/\/doi.org\/10.1016\/j.pocean.2015.12.014<\/span><\/a>\u00a0<\/span><\/h5>\n
Viglione, G. (2021, Mai 5). Fevers are plaguing the oceans \u2014 and climate change is making them worse. <\/span>Nature<\/span><\/i>, 593, 26-28. <\/span>doi: https:\/\/doi.org\/10.1038\/d41586-021-01142-4<\/span><\/h5>\n

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