Orbitolinopsis cenomaniensis n. sp., a new larger benthic foraminifera (Orbitolinidae) from the middle-?late Cenomanian of the Sarvak Formation (SW Iran, Zagros Zone): a regional marker taxon for the Persian Gulf area and Oman

2020 ◽  
Vol 67 ◽  
pp. 100413 ◽  
Author(s):  
Felix Schlagintweit ◽  
Mohsen Yazdi-Moghadam
2020 ◽  
pp. 57-67
Author(s):  
Felix Schlagintweit ◽  
Koorosh Rashidi

new larger benthic foraminifera is described as Broeckinella hensoni from the upper Maastrichtian Tar-bur Formation of SW Iran (Zagros Zone). In comparison to the type species of the genus, Broeckinella arabica Henson, which also occurs in the Tarbur Formation, the new species has distinctly larger dimensions (e.g., size and thickness of test, chamber height). The first record of a microspheric specimen of B. arabica shows previously unrecorded annular chambers in the final test stage. Therefore, the generic diagnosis is herein emended. In the Tarbur Formation, both B. hensoni n. sp. and B. arabica occur in foraminiferal-algal wackestones. However, B. arabica occurs in a wider range of microfacies, including packstones and grainstones. It is assumed that Broeckinella originated in the Upper Cretaceous with Broeckinella neumannae Gendrot. The upper Albian Broeckinella aragonensis Peybernès is herein transferred to the porcellaneous genus Peneroplis Montfort.


2020 ◽  
pp. 51-61 ◽  
Author(s):  
FELIX SCHLAGINTWEIT ◽  
KOOROSH RASHIDI

A new larger benthic foraminifera is described as Broeckinella hensoni from the upper Maastrichtian Tarbur Formation of SW Iran (Zagros Zone). In comparison to the type species of the genus, Broeckinella arabica Henson, which also occurs in the Tarbur Formation, the new species has distinctly larger dimensions (e.g., size and thickness of test, chamber height). The first record of a microspheric specimen of B. arabica shows previously unrecorded annular chambers in the final test stage. Therefore, the generic diagnosis is herein emended. In the Tarbur Formation, both B. hensoni n. sp. and B. arabica occur in foraminiferal-algal wackestones. However, B. arabica occurs in a wider range of microfacies, including packstones and grainstones. It is assumed that Broeckinella originated in the Upper Cretaceous with Broeckinella neumannae Gendrot. The upper Albian Broeckinella aragonensis Peybernès is herein transferred to the porcellaneous genus Peneroplis Montfort.


The Holocene ◽  
2016 ◽  
Vol 27 (4) ◽  
pp. 613-620 ◽  
Author(s):  
Frieda Bogemans ◽  
Mathieu Boudin ◽  
Rindert Janssens ◽  
Cecile Baeteman

The early- and mid-Holocene deposits of the Lower Khuzestan plain at the north-eastern margin of the Persian Gulf have been investigated by means of facies analysis of sediment successions of undisturbed cores. Organic material and molluscs have been selected for dating by radiocarbon whereby possible contamination by hard-water effect is discussed. The results suggest that the Holocene transgression in Mesopotamia may have taken place later than generally accepted. Before ca. 7700–7900 yr cal. BP, the plain was characterized by mud-dominated fluvial systems. During the mid-Holocene, tides invaded the existing valleys, and the sedimentary environment shifted from fluvial to estuarine but not as extensively as has previously been suggested. The estuarine environments lasted for about 2000–2500 years until ca. 4850–5000 yr cal. BP when the seaward part of the plain was again characterized by widespread fluvial sedimentation.


2021 ◽  
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>


Sign in / Sign up

Export Citation Format

Share Document