Red algae-bearing benthic foraminifera adapted to extremely warm temperatures and high salinity in the Persian Gulf 

Author(s):  
Christiane Schmidt ◽  
Katharina Neumüller ◽  
Raphael Morard ◽  
Hildegard Westphal ◽  
Gurjit Theara ◽  
...  

<p>The Persian Gulf hosts corals reefs under the most extreme conditions in the world, where summer maxima reach >36°C in combination with high salinities >44 PSU. While high bleaching thresholds characterize corals on these reefs, knowledge of adaptation of other calcifiers to local conditions is lacking. Benthic foraminifera are important calcifiers for coral reefs ecosystems as they build calcium carbonate tests. To map the environmental envelopes and the physiological limits of dispersal of benthic foraminfera, we exposed adult and juvenile foraminifera to a range of temperature and salinity conditions. Samples were collected from two reefs in the southern Gulf of Abu Dhabi, UAE. The dominant symbiont-bearing foraminifera was <em>Peneroplis planatus</em> hosting the endosymbiotic red algae <em>Porphyridium purpureum</em>. This was a surprising finding of sampling in these extreme reefs, as other symbiont-bearing benthic foraminifera are normally more abundant, but were completely absent in the reefs investigated. In the laboratory, we exposed <em>P. planatus </em>to 27°C (control), 35°C local summer maxima, and 39°C, +4°C above summer maxima, each with and without sediment substrates. The ecophysiological parameters growth, survivorship and photophysiological performance were measured. Photosynthetic rates declined after one week of exposure to 35°C and symbionts were photoinhibited at 39°C. Conditions were clearly more hostile for the symbionts, as host survival was high and growth rates unaffected by temperature. We hypothesize that to sustain growth the holobionts gained energy through heterotrophy under these conditions. In a second experiment, we exposed asexually reproduced offspring to an orthogonal temperature and salinity stress treatment (27-39°C, x 34-42 PSU) for four weeks. Asexual reproduction occurred in several treatments but was reduced under high salinity and temperature and combination of both parameters. The higher rate of asexual reproduction at control conditions indicates that stressful conditions do not trigger asexual reproduction in <em>P. planatus</em>, but rather suppress it. The results indicate that <em>P. planatus</em> can resist temperatures above current summer maxima for short periods of time, but that reproduction is impaired. Such heat-adapted populations may be considered a refuge for colonizing an increasingly warming Indian Ocean. Reproductive declines in the local population with increased warming threatens the long-term viability of this uniquely adapted organism.</p>

2015 ◽  
Vol 12 (6) ◽  
pp. 2743-2782
Author(s):  
P. L'Hégaret ◽  
X. Carton ◽  
S. Louazel ◽  
G. Boutin

Abstract. The Persian Gulf produces a high salinity water (Persian Gulf Water, PGW hereafter) flowing into the Sea of Oman, in the northwestern Indian Ocean. Past the Strait of Hormuz, the PGW cascades down the continental slope and spreads in the Sea of Oman under the influence of the energetic mesoscale eddies with different thermohaline signatures and pathways depending of the season. In spring 2011, the Phys-Indien experiment was carried out in the Arabian Sea an in the Sea of Oman. This study uses the results from the measurements to characterize the water masses, their thermohaline and dynamical signatures. During the spring intermonsoon, an anticyclonic eddy is often observed at the mouth of the Sea of Oman. This structure was present in 2011 and created a front between the eastern and western part of the basin. As well two energetic gyres were present along the Omani coast in the Arabian Sea. At their peripheries, injections of fresh and cold water are found in relation with the stirring of the eddies. The PGW observed below or between these eddies have a different dilution depending of the position and formation periods of the gyres. Furthermore, in the western Sea of Oman, the PGW is fragmented in filaments and submesoscale eddies. As well, recirculation of the PGW is observed, thus having the presence of salty nearby patches with two densities. Offshore, in the Arabian Sea, a submesoscale lens was recorded. The different mechanisms leading to its formation and presence are assessed here.


1917 ◽  
Vol 83 (2146supp) ◽  
pp. 100-101
Author(s):  
Edwin E. Calverley

2020 ◽  
Vol 2 (7) ◽  
pp. 191-196
Author(s):  
K. V. TIMAKHOV ◽  

The events that took place in the first half of 2020 once again demonstrated how countries in the modern globalizing world are interdependent and interconnected: what is happening in one part of the planet inevitably affects other states, regardless of their geographical position. The Kingdom of Saudi Arabia is no exception. The crisis that arose because of the outbreak of the coronavirus infection hit the country’s infant economic system, disrupting the government’s ambitious plans to modernize and transform the kingdom. In this connection, it is of great scientific interest to study changes in the internal political course of the monarchy of the Persian Gulf, consider and analyze feasible scenarios for the further development of the country.


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