Les algues calcaires du crétacé supérieur des rides de Villagrains,Landiras et Roquefort,Creon (Aquitaine centrale)

The lower Senonian of Central Aquitaine includes few calcareous algae, alone green algae, while the upper Senonian admits nothing but numerous red algae.A new species has been discovered (Lithothamnium villaegranis n. sp.). Solenomeris, generally frequent in the Paleocene deposits, has been identified in the maestrichtian levels.     

Early Cretaceous calcareous algae from central Iran (Taft Formation, south of Aliabad, near Yazd)

A rich association of calcareous algae is described from the Lower Cretaceous (Barremian–? Lower Aptian) deposits of the Taft Formation, located south of Aliabad (in the vicinity of Yazd, central Iran). The association mainly consists of dasycladaleans and bryopsidales (udoteaceans and gymnocodiaceans); additionally, rare “solenoporaceans” and cyanophyceans are present. Three new species are described: two are dasycladaleans (Pseudoactinoporella? iranica and Holosporella farsica) and one is an udoteacean (Boueina minima). Many of the described and illustrated algae are mentioned for the first time from Iran.     

Prasinophyte green algae <Emphasis Type="Italic">Tasmanites</Emphasis> and problematic fossils in the Upper Vendian Biota of the Zavkhan Basin,western Mongolia

A new species of spheromorphic microfossils of Tasmanites with a characteristically thick cover is established in the Zavkhan association of algae, microfossils, and problematic Upper Vendian organisms from the upper part of the siliciclastic–carbonate section of the Tsagaanolom Formation (632 ± 14 Ma) of the Zavkhan Basin in western Mongolia. Representatives of this genus are widespread in the Phanerozoic beds and their accumulations are recorded in the Domanik facies and near hydrocarbon deposits.     

Habitats and probable nature of acritarchs from the Upper Riphean Chencha Formation

Morphology and taphonomy of acritarchs from the Upper Riphean deposits of the Baikal Folded Region (eastern Siberia) are analyzed. The morphotypes of acritarchs are compared to various stages in the life cycle of modern green algae of the order Chlorococcales. The acritarchs Dictyotidium minor Stan. and the modern coenobial taxon Pediastrum boryanum (Turp). Menegh. showed the greatest similarity of structure.     

Non-calcified macroalgae from the lower Famennian (Upper Devonian) of the Holy Cross Mountains,Poland

Non-calcified algal remains were collected from the lower Famennian deposits at the Kowala quarry in the Holy Cross Mountains, central Poland. Each specimen is represented solely by vegetative organs. On the basis of the material collected, a new algal genus and species has been formally erected. Vittella dixii nov. gen., nov. sp. (Order ?Bryopsidales) includes thalli consisting of long bundles of hair-like filament structures arranged in parallel fashion to the thallus length. Some other algal remains are regarded as Inocaulis-like forms. They possess long, flat blades with entire margins, and are ornamented with very dense, hair-like projections. The rest of the specimens found so far has been illustrated and tentatively classified as probably belonging to either Bryopsidales or Dasycladales algae. The exceptional preservation of the non-calcified algal thalli investigated suggests that special taphonomic conditions have prevailed during sedimentation of the lower part of the Famennian Kowala section. These may have involved rather rapid burial in oxygen-restricted (dysoxic and anoxic) sea-bottom environment, inhibiting the activities of scavengers and bioturbators, as well as oxidative degradation. The preservation of the algae, together with sedimentological and geochemical characteristics of the host rocks indicate that they rather represent parautochthonous assemblage, buried close to their natural habitat.     

Palaeoaplysinella gen. nov. and Likinia Ivanova and Ilkhovskii, 1973 emend., from the type Moscovian (Russia) and the algal affinities of the ancestral palaeoaplysinaceae n. comb

Because of the cellular tissue often described and occasionally confused in the literature with some Archaeolithophyllum, an assignment to the red algae Archaeolithophyllaceae is proposed for Palaeoaplysinaceae nomen translat., herein. Archaeolithophyllaceae, Palaeoaplysinaceae and several “phylloid algae” might compose the order Archaeolithophyllales nom. translat. A new ancestral form of the primitive paleoaplysinaceans is described in the Podolskian (early late Moscovian) of the Moscow Basin, under the name Palaeoaplysinella n. gen. with P. moscovica n. sp., as type species. These forms, proportionally small, do not construct reefal structures, and is reworked in bioclastic grainstone rich in algae and fusulinids. Its structure differs from the following late Moscovian forms previously described as palaeoaplysinaceans: (a) Likinia from the Podolskian-Myachkovian deposits of the Moscow basin and (b) the Desmoinesian palaeoaplysines mentioned in Utah (USA) (a taxon to re-describe). Likinia is revised herein. Its type species does not belong to the palaeoaplysinaceans; nevertheless, its assignment is uncertain. Since their origin, the Palaeoaplysinaceae colonized the shelf seas of the northern subtropical to warm-temperate provinces (from 15 to 45°N) including the Urals, Greenland, Canadian Arctic Archipelago, some parts of the North American Craton and the Klamath Exotic Terrane (California). The adjacent regions of the southern USA, northern Mexico (Sonora), Pericaspian, and Donbass have not been colonized. The history of Palaeoaplysinacea is probably linked to the evolution of the Ural Ocean. Based on these reconstructed paleolatitudes, the Akiyoshi Terrane in Japan, which contains rare Palaeoaplysina, was emplaced between 15 and 45° North latitude during the Asselian (earliest Permian).     

Paleoecologic and stratigraphic significance of the freshwater algae <Emphasis Type="Italic">Pediastrum</Emphasis> in the Upper Cretaceous (Turonian) marine deposits,north Western Desert,Egypt

Palynological investigations of samples collected from the Abu Roash Formation, Faghur Hj5-1 well, north Western Desert, Egypt show a low diversity in palynomorph assemblage. This assemblage is mainly dominated by a clear proliferation of Pediastrum (and other allied algal forms, e.g., Scenedesmus and Botryococcus) which today lives exclusively in freshwater. Such a prominent record within the current marine deposits could be considered a good biostratigraphic datum in the Upper Cretaceous (Turonian) period rather than an ecologic event in the north Western Desert, Egypt. The influence of freshwater input on the studied deposits is proven by the presence of heavy minerals including kyanite, zircon, staurolite, and amphiboles encountered in siliciclastic sediments. Most of these minerals are sub-rounded to rounded so they were derived probably from sedimentary rocks. In the studied succession, the presence of Pediastrum reflects sea level fall (i.e., lowstand systems tracts). The occurrence of Pediastrum and other algae in such marine deposits reflects the predominant deposition of fluviatile sediments related to the discharge of rivers into shelf seas.     

Representatives of the genus Triploporella (Dasycladales, calcareous algae) in the Lower Cretaceous limestones of Romania

Recent studies on the Lower Cretaceous deposits located in various areas of the Romanian Carpathians resulted in the identification of several specimens of dasycladalean algae assigned to the genus Triploporella including Triploporella carpatica Bucur, Triploporella cf. praturlonii Barattolo, Triploporella cf. steinmannii Barattolo, Triploporella sp. 1, Triploporella sp. 2, and Triploporella n. sp. This paper provides arguments on their taxonomic assignment, together with discussions on the Triploporella species described in the literature and their paleobiogeographic significance.     

Terrestrial lithophilic algae in a granite canyon of the Teteriv River (Ukraine)

Sixty-eight species of algae were found on granite outcrops of a canyon of the Teteriv River in the forest zone of Ukraine (Cyanoprokaryota 1 species, Chlorophyta 49, Streptophyta 11, Xanthophyta 2, Eustigmatophyta 1, Bacillariophyta 4). Two of these are new records for the flora of Ukraine [Spirotaenia bryophila (Brébisson) Lütkemüller and Coelastrella multistriata (Trenkwalder) Kalina et Pun?ochá?ová] and several are rare and interesting species [Stichococcus mirabilis Lagerheim, Dictyochloropsis splendida Geitler, D. reticulata (Tschermak-Woess) Tschermak-Woess, Mesotaenium macrococcum (Kützing) Roy et Bisset, M. chlamydosporum De Bary, Klebsormidium cf. bilatum Lokhorst]. The species composition of algae of this granite canyon was characterized by the following specific features: a high diversity of green algae (mainly trebouxiophycean and streptophycean algae); a considerable species diversity and abundance of green conjugating algae among the mentioned streptophycean algae; a low species diversity of cyanoprokaryotes, as well as the presence of the genera Mesotaenium Nägeli and Trentepohlia Martius in the dominating complex. Two slopes of the canyon with different expositions and plant cover were characterized by different proportions of epilithic and chasmoendolithic groups of algae as well as different dominating complexes. The species composition of algae from granite canyon of forest zone was the most similar to the more humid and shaded habitats of a granite canyon of steppe zone of Ukraine studied previously.     

Litho- and biostratigraphy of the Upper Jurassic Mozduran Formation,Kopet-Dagh,Iran, and its paleoenvironmental implications

The Upper Jurassic Mozduran Formation at Baghak section, Kopet-Dagh area northeast Iran, characterized by multiple units of carbonates and evaporates intercalated with siliciclastic deposits, yielded benthic foraminifera, calcareous algae, and crustacean coprolites, including Alveosepta jaccardi, Charentia aff. nana, Deloffrella quercifoliipora, Marinella cf. lugeoni, Favreina, and Solenopora sp. The almost consistent occurrence of Alveosepta jaccardi in the studied section, i.e., the Alveosepta jaccardi Zone, indicates late Oxfordian to the Kimmeridgian in age. Facies analysis of the formation reveals depositional settings of a peritidal zone, a lagoon, and a high-energy shoal of a carbonate ramp. Terrigenous and evaporites are found in eastern parts of Kopet-Dagh, representing a more proximal sedimentary environment. These siliciclastic inputs are associated with tectonic events during Oxfordian to Tithonian in the region.     

The brachiopod family Linoproductidae stehli from the lower Moscovian of the Middle Carboniferous of the Moscow Region

The phylogeny and taxonomy of the brachiopod family Linoproductidae are revised. The change in the distributional pattern of spines and distinctive structure of the median lobe of the cardinal process are shown to be the main apomorphies in the family evolution. A new subfamily, Linispininae, and the included new genera, Linispinella and Linispinus, are described. In the nominotypical subfamily Linoproductinae, a new genus Linoproductoides and two new species included in this genus are described from the Vereiskian deposits of the Moscow Region. The new species Linispinus riparius (Trautschold), L. longus sp. nov., and L. staricensis (Ivanov) are described from the Kashirskian deposits. Another new species is tentatively described as “Linoproductus” kabanovi.     

从塔北隆起奥陶纪钙藻化石探讨奥陶纪的古环境

塔里木盆地塔北隆起轮南46井、英买1、2井奥陶纪石灰岩内含有大量的钙藻化石、蓝细菌以及疑难微体化石。这些钻井岩芯均在深达5000-6200m的地下深部取得。钙藻主要为绿藻类的Dasyporella,Ver‘miporella,Moniliporella以及?Plexa;红藻类的管孔藻类Solenoporaceans;钙化蓝细菌则有Girvanella,Botomaella,?Subtifloria等;疑难微体化石有Bevocastria,Nuia,Rothpletzella。这些钙藻生活于热带或亚热带正常盐度的浅海水内,其水深不到20m。世界各地的奥陶纪Vermiporella均位于古赤道的两侧,这表明它们是在气候炎热、温暖海水中生活的一类海洋藻类。Girvanella以藻灰结核和内碎屑最为常见,某些球粒可能代表Girvanella破碎后形成的单管或小棒。塔里木盆地钙藻植物群相似于哈萨克斯坦、波罗的海周围地区以及北美同时代植物群,这表明这些钙藻和蓝细菌化石具有遍布于全球的性质。塔北隆起早、中奥陶世沉积属于典型的碳酸盐岩台地相沉积。到晚奥陶世时,碳酸盐岩沉积被浅水陆棚沉积所取代,以陆源碎屑岩为主,夹少量的碳酸盐岩。     

Effects of depth, sediment and grazers on the degradation of drifting filamentous algae (Cladophora glomerata and Pilayella littoralis)

Eutrophication in the northern Baltic Sea promotes growth of annual filamentous algae. The algae detach, gather at the bottom and give rise to algal mats of varying size, density, composition and condition. Dense mats of filamentous algae induce anoxia, which in turn leads to faunal mortality. By a set of field experiments, we have studied the fate of the abundant Cladophora glomerata after detaching from the rocky substrate, and the effect of water depth and sediment on its decay. Further, we have studied the importance of common mesograzers (Gammarus and Idotea) on the rate of degradation of C. glomerata and Pilayella littoralis.Our results show that loose algae at shallow sites (8 m) decompose faster than algae in deeper (18 m) areas. Drifting C. glomerata on the sediment is more rapidly broken down and dissolved than algae floating in the water column, which depends on higher microbiological activity. Dominant amphipods (Gammarus spp) colonise near-shore drift algae quickly, and juvenile bivalves (Cerastoderma glaucum) utilise algae in the water column for settling. Moderate natural densities of grazers (Gammarus spp and Idotea baltica) in the drifting algae did not increase the degradation rates of C. glomerata and P. littoralis. C. glomerata was completely decomposed in 4 months.Our experiments demonstrate the effects of position (depth, water/sediment) and grazing on the degradation of drifting filamentous algae. Mass developments of opportunistic algae occur annually in the study area, and information on the destiny of detached drift algae may help us to predict their longevity and the damage they cause, and hence, to decide on long-term measures needed to improve environmental conditions.     

Elucidating the composition and conservation of the autophagy pathway in photosynthetic eukaryotes

Aquatic photosynthetic eukaryotes represent highly diverse groups (green, red, and chromalveolate algae) derived from multiple endosymbiosis events, covering a wide spectrum of the tree of life. They are responsible for about 50% of the global photosynthesis and serve as the foundation for oceanic and fresh water food webs. Although the ecophysiology and molecular ecology of some algal species are extensively studied, some basic aspects of algal cell biology are still underexplored. The recent wealth of genomic resources from algae has opened new frontiers to decipher the role of cell signaling pathways and their function in an ecological and biotechnological context. Here, we took a bioinformatic approach to explore the distribution and conservation of TOR and autophagy-related (ATG) proteins (Atg in yeast) in diverse algal groups. Our genomic analysis demonstrates conservation of TOR and ATG proteins in green algae. In contrast, in all 5 available red algal genomes, we could not detect the sequences that encode for any of the 17 core ATG proteins examined, albeit TOR and its interacting proteins are conserved. This intriguing data suggests that the autophagy pathway is not conserved in red algae as it is in the entire eukaryote domain. In contrast, chromalveolates, despite being derived from the red-plastid lineage, retain and express ATG genes, which raises a fundamental question regarding the acquisition of ATG genes during algal evolution. Among chromalveolates, Emiliania huxleyi (Haptophyta), a bloom-forming coccolithophore, possesses the most complete set of ATG genes, and may serve as a model organism to study autophagy in marine protists with great ecological significance.     

New insights into diversity and selectivity of trentepohlialean lichen photobionts from the extratropics

Aerial green algae of Trentepohliaceae can form conspicuous free-living colonies, be parasites of plants or photobionts of lichen-forming ascomycetes. So far, their diversity in temperate regions is still poorly known as it has been mostly studied by phenotypic approaches only. We present new insights in the phylogenetic relationships of lichenized representatives from temperate and Mediterranean parts of Europe by analysis of 18S rRNA and rbcL gene fragments, and nuclear ITS sequence data. For this purpose we isolated the trentepohlialean photobionts from lichens representing different genera. Algal cultures from lichenized and free-living Trentepohliaceae were used to design new primers for amplification of the marker loci. We constructed a phylogenetic hypothesis to reveal the phylogenetic placements of lichenized lineages with 18S rRNA and rbcL sequences. ITS variation among the clades was substantial and did not allow including them in the general phylogenetic assessment, yet ITS appears to be a promising marker for DNA-barcoding approaches. Specific algae were found in particular lichen but the overall diversity of photobionts was limited. The multilocus tree does not support the current morphological classification of genera in Trentepohliaceae, suggesting that morphology is more variable than previously thought in this group of algae.     

Cyclocrinitids from the Lower Palaeozoic Tethyan sequence of Spiti,India

Well preserved cyclocrinitids (calcareous green algae) are reported from early Palaeozoic deposits of Spiti, Himachal Pradesh, India. Casts of the algal fossils are preserved in calcareous grey siltstone unit of the Takche Formation (Late Ordovician–Early Silurian) which appears rusty/earthy brown due to weathering. The assemblage includes Cyclocrinites favus, Cyclocrinites pyriformis, Cyclocrinites cf. welleri, Cyclocrinites sp. and Cyclocrinites globosus. Both Cyclocrinites cf. welleri and Cyclocrinites globosus are reported for the first time from the entire Tethyan Himalaya, India. The described algal flora basically denotes relatively shallow marine depositional setting and low to moderate hydrodynamic conditions.     

Macroscopic plant remains from the base of the Ust’-Pinega formation (Upper Vendian of the Arkhangelsk Region)

Plant macrofossil remains from the Lyamtsa and Arkhangelsk beds of the Ust’-Pinega Formation (Vendian) are reported for the first time. Three new taxa of vendotaenid algae showing cellular parenchymatous morphology are described: Archyfasma lamellata sp. nov., Favosiphycus wukii gen. et sp. nov., and Gandvikia caudata gen. et sp. nov. Phytostratigraphic characteristics allow the author to correlate the deposits under study with the base of the Mogilev Formation (Vendian of Podolia). A distinctive Lower Redkino vendotaenid flora is described for the first time. It is shown to precede the Upper Redkino Eoholynialen flora.     

Localization of attachment area of the symbiotic Chlorella variabilis of the ciliate Paramecium bursaria during the algal removal and reinfection

Chlorella spp. and ciliate Paramecium bursaria share a mutual symbiosis. However, both alga-removed P. bursaria and isolated symbiotic algae can grow independently. Additionally, mixing them experimentally can cause algal reinfection through host phagocytosis. Although the symbiotic algal localization beneath the host cell cortex is a prerequisite phenomenon for maintenance of the relationship of their endosymbiosis, how and where the algae locate beneath the host cell cortex remains unknown. To elucidate this phenomenon, algal distribution patterns during algal removal and reinfection were observed. During algal removal, algae at the host anterior cortex were easier to remove than at the posterior and ventral or dorsal cortex areas. During algal reinfection, the algae after separation from the host digestive vacuoles tended to localize beneath the host ventral or dorsal cortex more readily than that at other cortices. Algae that reinfected trichocyst-removed paramecia didn’t show this localization. Trichocyst-discharge experiments clarified that trichocysts of the anterior cortex are difficult to remove. In 14 strains of P. bursaria, some of the paramecia lacked their symbiotic algae at the anterior cortex. These observations demonstrate that symbiotic algae of P. bursaria are difficult to localize at the anterior cortex and that they are easy to remove from the area.     

The effects of nutrient enrichment and herbivore abundance on the ability of turf algae to overgrow coral in the Caribbean

Turf algae are multispecies communities of small marine macrophytes that are becoming a dominant component of coral reef communities around the world. To assess the impact of turf algae on corals, we investigated the effects of increased nutrients (eutrophication) on the interaction between the Caribbean coral Montastraea annularis and turf algae at their growth boundary. We also assessed whether herbivores are capable of reducing the abundance of turf algae at coral-algae boundaries. We found that turf algae cause visible (overgrowth) and invisible negative effects (reduced fitness) on neighbouring corals. Corals can overgrow neighbouring turf algae very slowly (at a rate of 0.12 mm 3 wk⁻¹) at ambient nutrient concentrations, but turf algae overgrew corals (at a rate of 0.34 mm 3 wk⁻¹) when nutrients were experimentally increased. Exclusion of herbivores had no measurable effect on the rate turf algae overgrew corals. We also used PAM fluorometry (a common approach for measuring of a colony''s “fitness”) to detect the effects of turf algae on the photophysiology of neighboring corals. Turf algae always reduced the effective photochemical efficiency of neighbouring corals, regardless of nutrient and/or herbivore conditions. The findings that herbivores are not capable of controlling the abundance of turf algae and that nutrient enrichment gives turf algae an overall competitive advantage over corals together have serious implications for the health of Caribbean coral reef systems. At ambient nutrient levels, traditional conservation measures aimed at reversing coral-to-algae phase shifts by reducing algal abundance (i.e., increasing herbivore populations by establishing Marine Protected Areas or tightening fishing regulations) will not necessarily reduce the negative impact of turf algae on local coral communities. Because turf algae have become the most abundant benthic group on Curaçao (and likely elsewhere in the Caribbean), new conservation strategies are required to mitigate their negative impact on coral communities.