A morphological, anatomical and palynological study of Aethionema lepidioides (Brassicaceae) - an endangered species endemic to Turkey

Aethionema lepidioides Hub.-Mor. is an endangered endemic species in Turkey with a very narrow natural distribution area. The present study aims to reveal the structural features of this species. For this purpose, its unknown morphological features – such as leaf, petal, sepal dimensions and shapes, filament and anther lengths, as well as seed dimensions, shape, colour and micromorphology – have been studied for the first time. To reveal the pollen characteristics of Ae. lepidioides, light microscope and SEM studies were conducted. Additionally, in the present study the anatomical features of Ae. lepidioides were also studied for the first time. The Ae. lepidioides leaves were found to be linear-oblanceolate, with an entire margin and a subacute to obtuse apex. The seeds were found to be dark brown and oval-shaped, with reticulated surface ornamentation. Anatomical studies found roots in the secondary growth stage, with xylem-filled pith. The stem was in the primary growth stage, featuring a multi-layer cortex under its outermost single-layered epidermis, a pronounced endodermis and a central cylinder beneath. The leaves were thick, amphistomatic and covered with a prominent wax layer. Their mesophyll was equifacial, and their stoma type was anisocytic. A stomatal index of 26 was found for the upper epidermis, while a corresponding index of 28.4 was found for the lower epidermis. The pollens were monad, radially symmetrical and isopolar. The pollen type was colpate, and the pollen shape was found to be prolate-spheroidal with a P/E ratio of 1.08.

New results of a palynological study of the Lake Doroninskoe sediments (Eastern Siberia, Transbaikalia)

This article presents the results of the study of the bottom sediments of the meromictic Lake Doroninskoe. For the study, the method of spore-pollen analysis was used. The record showed that during the accumulation of 65 cm of the sediment layer in the Chita-Ingodinskaya depression, pine and larch predominated along the ridges, with steppe and meadow associations in the lower parts of the depression. According to regional correlations, the distribution of light-coniferous-taiga vegetation in Transbaikalia occurred as early as the Middle Holocene, and it did not undergo cardinal changes until modern times. According to these data, sediments may have accumulated during this time period.

Results of Archaeoparasitological and Palynological Analyzes of the Contents of the Sewage Drain of the Chorgun Tower (South-Western Crimea)

The article presents the results of an archaeoparasitological and palynological study of a sample taken from the sewage drain of the Chorgun Tower. This is a fortification on the territory of the village of Chernorechie (South-Western Crimea). According to archaeological research, the construction of the keep dates back to the third quarter of the 15th century. Four types of eggs of intestinal parasites infecting humans and synanthropic animals were identified in the sample. Regarding parasitic and infectious gastrointestinal diseases, human whipworm and roundworm eggs found in the sample are indicative of relatively unfavorable sanitary conditions of the fortification. Based on the features of the archaeoparasitological spectrum, it can be concluded that anthelminthic agents were used or food with antiparasitic effects against roundworms was consumed. The difficult sanitary and epidemiological situation was also complicated by synanthropic rodents, such as rats and domestic mice, which could be a constant source of dangerous infections in the Chorgun Keep. A palynological study of the contents of the sewage runoff made it possible to obtain additional information on the nutrition of people who used the latrine facilities in the Chorgun Keep. What is equally important is that the study demonstrates the possibilities of methods for the study of canalization as a source of bioarchaeological information.

Aspects from the evolution of past vegetation in Southern Transylvania (Sibiu region)

The article reviews the results obtained through the palynological study of sequences obtained from the Sibiu region and adjacent areas. The oldest Upper Pleistocene sequences we refer to seem to reflect snapshots from the Last Glacial Maximum. The history of the Late Glacial and Holocene vegetation here is broadly part of the succession known for the territory of Romania, in the Carpathians and the surrounding areas of medium and low altitudes. The dynamics of the main forest and grasses taxa were highlighted, influenced both by natural factors and, more recently, by human activity. The reference area is characterized by the domination of the forests during the interstadials and by open landscape of forested steppe during the cold, stadial periods.

Source Rocks’ Potentiality of the Sargelu Formation (Middle Jurassic) in the Taq Taq Oilfield, Kurdistan Region, Iraq

Thirty rock samples were selected from the well Tq-1 that penetrated the Jurassic beds in the Taq Taq Oilfield to be studied the source rock potentiality of the Sargelu Formation. The formation is characterized by three types of microfacies, namely, foraminiferal packstone, grainstone microfacies, fossiliferous packstone microfacies, and foraminiferal wackestone which were deposited in an environment extending from middle to outer carbonate ramp. An average of 3.03 wt.% of total organic carbon was obtained from a Rock Eval pyrolysis analysis carried out on 24 selected rock samples. The petrographic analysis for such organic matters revealed that they are of kerogen types III and IV and they are currently in a post-mature state. Pyrolysis parameters showed that limited generation potential was remained for these sources to expel generated hydrocarbons. The palynological study showed that Amorphous Organic Matter forms the highest percentage of organic matter components with more than 70%, followed by phytoclasts with 10 – 25 % and palynomorphs of less than 10%. The organic matters within the Sargelu Formation are deposited at the distal part of the basin under suboxic to anoxic condition. The color of the organic matter components, examined under transmitted light, showed Thermal Alteration Index values between 3+ and 4-. Such values may indicate that these organic matters are thermally at the end of the liquid oil generation zone and beginning of condensate-wet gas generation zone. The thermal maturity of the Sargelu Formation depending on the calculated VRo% revealed that the formation in the studied oilfield is currently at the peak of the oil generation zone. The Sargelu Formation in the studied field is considered as an effective source rock, as it has already generated and expelled hydrocarbons.

POLLEN MORPHOLOGY OF LYCIUM (SOLANACEAE) SPECIES IN IRAN

Lycium (Solanaceae) has more than 100 species in arid and semi-arid parts of the world. In Iran, this medicinal plant is represented by 6 species, on which no palynological study has been conducted. Pollen morphology of 7 taxa are considered for the first time to evaluate the species relationships based on palynological data. Observations were made by use of Scanning electron microscopy on untreated pollen grains. Multivariate statistical analyses were carried out for qualitative and quantitative pollen features in the species studied. Results show that all pollen grains were monad, isopolar, zonotricolporate in prolate and preprolate shape. Exine sculpture was of striate and regulate patterns. Variations in pollen grains are considered to overcome the identification problems in species separation in morphologically similar taxa in this genus in Iran. The importance of pollen features in delimitation in some genera of Solanaceae was previously proven and the present study elucidates that some features as exine sculpture and some quantitative characters are of diagnostic importance in Lycium species native to Iran.

Miocene Palynology of the Solimões Formation (Well 1-AS-105-AM), Western Brazilian Amazonia

During the Miocene, Andean tectonism caused the development of a vast wetland across western Amazonia. Palynological studies have been the main source of chronological and paleobotanical information for this region, including several boreholes in the Solimões Formation in western Brazilian Amazonia. Here, a palynological study of well core 1-AS-105-AM drilled in Tabatinga (Amazonas, Brazil) is presented: 91 new taxa are erected (25 spores and 66 pollen, including one new genus), 16 new combinations are proposed, and a list of botanical/ecological affinities is updated. We recorded 23,880 palynomorphs distributed in 401 different types. Among pollen and spores, 62 extant families and 99 extant genera were identified, which accounts for 39% and 30% of known botanical affinities to the family and genus level, respectively. Individual samples have pollen/spore counts with approximately 25% to 95% of known affinities to the family level. Pollen associations are sourced primarily from the wetland environments and to a minor extent from nonflooded forests. Palynological diversity analyses indicate an increase from the early to the middle/early late Miocene in core 1-AS-105-AM. Probable scenarios to explain this diversity increase include a higher degree of environmental complexity from the middle Miocene onwards, that is, a more heterogeneous riverscape, including broader extensions of nonflooded forests, as opposed to the swamp-dominated early Miocene. Additionally, the positive effects of the Miocene Climatic Optimum on plant richness could explain the increase in pollen richness. We posit hypotheses of forest diversification that can be tested as more botanical affinities are established along with a longer Miocene record.

Palinologia de turfas do alto curso do Arroio Cará, Coxilha Rica, Santa Catarina, Brasil

Palynology of peaty sediments from the high course of Cará Brook Creek, Coxilha Rica, Santa Catarina, Brazil. This paper presents the results of the palynological study of a sedimentary core collected in a bog in the upper part valley of Cará Brook Creek, in the cultural territory of Coxilha Rica, located in the Campos Gerais Plateau in Santa Catarina, Southern Brazil. The base of the core was dated in 6.900 14C years BP (7,845–7,690 cal years BP). The identification of the palynomorphs and the cluster analysis made possible to define two distinct palynological phases, despite the predominance of grassland vegetation throughout the whole core. From 34 cm, the frequency of bryophytes decreases, accompanied by the increase of the diversity of all vegetal taxa. Throughout the core, the most frequent families are Poaceae, Cyperaceae Apiaceae. The results indicate that the landscape of the upper course of the Brook Creek was characterized by grasslands from 6,900 14C years BP under a regional and humid climate, with a temperature increase in the historical period. Keywords: Middle Holocene, palynomorphs, grasslands, Araucaria forest, Highland.