Subjects -> PALEONTOLOGY (Total: 43 journals)
Showing 1 - 21 of 21 Journals sorted by number of followers
Journal of Quaternary Science     Hybrid Journal   (Followers: 31)
Quaternary Science Reviews     Hybrid Journal   (Followers: 26)
Quaternary Research     Full-text available via subscription   (Followers: 19)
Palaeontology     Hybrid Journal   (Followers: 17)
Palaeogeography, Palaeoclimatology, Palaeoecology     Hybrid Journal   (Followers: 13)
Peer Community Journal     Open Access   (Followers: 13)
Boreas: An International Journal of Quaternary Research     Hybrid Journal   (Followers: 13)
Geologica Saxonica     Open Access   (Followers: 12)
Historical Biology: An International Journal of Paleobiology     Hybrid Journal   (Followers: 9)
Facies     Hybrid Journal   (Followers: 9)
Journal of Vertebrate Paleontology     Full-text available via subscription   (Followers: 8)
Journal of Paleontology     Hybrid Journal   (Followers: 8)
Paleobiology     Full-text available via subscription   (Followers: 6)
Alcheringa: An Australasian Journal of Palaeontology     Hybrid Journal   (Followers: 6)
Journal of Paleolimnology     Hybrid Journal   (Followers: 5)
European Journal of Protistology     Hybrid Journal   (Followers: 5)
Fossil Record     Open Access   (Followers: 5)
Paleoceanography and Paleoclimatology     Full-text available via subscription   (Followers: 5)
EvoDevo     Open Access   (Followers: 4)
Swiss Journal of Palaeontology     Hybrid Journal   (Followers: 4)
Annales de Paléontologie     Full-text available via subscription   (Followers: 4)
Paläontologische Zeitschrift     Hybrid Journal   (Followers: 4)
Paleontological Journal     Full-text available via subscription   (Followers: 4)
Geobios     Full-text available via subscription   (Followers: 4)
Palaeontographica A     Full-text available via subscription   (Followers: 3)
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen     Full-text available via subscription   (Followers: 3)
International Journal of Speleology     Open Access   (Followers: 3)
Quaternaire     Open Access   (Followers: 3)
Palaeoworld     Hybrid Journal   (Followers: 3)
Marine Micropaleontology     Hybrid Journal   (Followers: 2)
Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy)     Open Access   (Followers: 1)
Vertebrate Anatomy Morphology Palaeontology     Open Access   (Followers: 1)
Palynology     Hybrid Journal   (Followers: 1)
Novitates Paleoentomologicae     Open Access   (Followers: 1)
Annals of Carnegie Museum     Full-text available via subscription   (Followers: 1)
Review of Palaeobotany and Palynology     Hybrid Journal   (Followers: 1)
PaleoBios     Open Access   (Followers: 1)
Zitteliana     Open Access  
Ameghiniana     Open Access  
Papers in Palaeontology     Hybrid Journal  
Spanish Journal of Palaeontology     Open Access  
Open Quaternary     Open Access  
Ichnos: An International Journal for Plant and Animal Traces     Hybrid Journal  
Revue de Micropaleontologie     Full-text available via subscription  
Comptes Rendus Palevol     Open Access  
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Facies
Journal Prestige (SJR): 0.669
Citation Impact (citeScore): 2
Number of Followers: 9  
 
  Hybrid Journal Hybrid journal (It can contain Open Access articles)
ISSN (Print) 1612-4820 - ISSN (Online) 0172-9179
Published by Springer-Verlag Homepage  [2469 journals]
  • Devonian to Carboniferous continental-scale carbonate turnover in Western
           Laurentia (North America): upwelling or climate cooling'

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      Abstract: Abstract The Devonian to Carboniferous (DC) transition coincided with a green-to-ice house climatic shift, anoxia, disappearance of lower latitude carbonate banks, and turnover from warm-to-cool water carbonate factories. In western Laurentia, the switch to carbonate factories dominated by cool-water biota was contemporaneous with a tectonically driven palaeogeographic change. To investigate this depositional shift and infer the relative impact of climate vs tectonics, a continental-scale sedimentological and geochemical study was conducted on twelve stratigraphic sections of DC strata from western Canada to southern Nevada (USA). The spatial–temporal distribution of microfacies records the turnover from [i] a Famennian lime mud-rich, shallow warm-water carbonate ramp with low sedimentation rates, mesotrophic conditions and tabular geometry to [ii] Tournaisian to Viséan lime mud-depleted and grainstone dominated cool-water carbonate ramp with anomalous high sedimentation rates, oligotrophic conditions and a pronounced slope. Positive excursions of δ18Ocarb (+ 2‰ V-PDB) and δ13Ccarb (+ 4‰ V-PDB) of Lower Mississippian carbonates likely correspond to the first cooling peak of the Carboniferous-Permian icehouse climate, following carbon withdrawal during black shale deposition during the late Famennian and early Tournaisian. However, late Tournaisian return of photozoan elements and their persistence throughout the Viséan suggests that warmer surface water existed, revealing a decoupling of the lower latitude ocean and the atmosphere. Shoaling of the thermocline was likely a result of cold-water upwelling along an open coast, as the Antler orogen no longer provided an oceanic obstruction to the west. This study shows that carbonate platforms are more susceptible to regional changes than global shifts.
      PubDate: 2022-07-25
       
  • Carbonate factory of Pietra di Finale coastal wedge (Miocene): the unusual
           abundance of stylasterids (Cnidaria, Hydrozoa)

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      Abstract: Abstract This work focuses on the carbonate factories constituting the Pietra di Finale Fm cropping out in the Ligurian Alps. This unit constituted a mixed carbonate–siliciclastic coastal wedge developed during the Middle Miocene. The carbonate factories characterizing the coastal wedge of the Pietra di Finale clearly differ from those of the coastal mixed systems and carbonate platforms developing during the Miocene elsewhere in the Mediterranean area. Here, in the Ligurian Alps, the euphotic carbonate factory does not show any evidence of seagrass meadows and coral bioconstructions. Zooxanthellate corals are present only as skeletal debris associated with abundant stylasterids. In the mesophotic and oligophotic zones, the typical oligophotic biota of red algae and larger benthic foraminifers are strongly reduced. The coastal wedge of the Pietra di Finale shows an unusual abundance of stylasterids, classically interpreted as deep-water biota. However, in this example, the absence of low-energy textures and other skeletal components suggest a shallow-water origin, probably in the eu- or mesophotic zone. The stylasterids colonized the hard substrates available and were successively removed and resedimented to form the skeletal fraction of the coastal wedge of the Pietra di Finale. The abundance of stylasterids is restricted to particular and limited situations in the Miocene of the Mediterranean, thus suggesting that their abnormal development is controlled by local rather than global factors.
      PubDate: 2022-06-21
       
  • Charophyte communities in Barremian Iberian wetlands

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      Abstract: Abstract A combined micropalaeontological, taphonomical and sedimentological study was carried out in the non-marine Barremian of the Maestrat Basin (E Iberian Chain) to elucidate the palaeoecology of Barremian charophytes. Understanding the palaeoecology of fossil charophytes is of prime importance for the accurate application of charophyte biozonations, since most species used as biostratigraphic markers and/or biozone index species are restricted to facies formed in a particular environment. Five charophyte biocoenoses were distinguished. (1) Charophyte association from freshwater alkaline lakes receiving low clastic input, mainly composed of Atopochara trivolvis var. triquetra, Clavator harrisii, Ascidiella stellata, and A. triquetra. The thalli known as Munieria grambastii, corresponding to Clavator utricles, were extremely abundant in the shallowest facies of the lake margins, and Hemiclavator-rich populations were also locally dominant. (2) An association characteristic of freshwater alkaline lakes with high clastic input was mainly composed of Echinochara lazarii, Globator maillardii var. trochiliscoides, A. trivolvis var. triquetra, C. harrisii, Hemiclavator neimongolensis var. neimongolensis, and locally also Clavator calcitrapus. (3) Monospecific populations of Porochara maestratica thrived in brackish settings with little clastic influence, whereas (4) monospecific E. lazarii populations thrived in clastic-influenced brackish settings. (5) A charophyte association grew in lakes that developed in mudflat to floodplain environments and was mainly constituted by E. lazarii, A. trivolvis var. triquetra, and C. harrisii var. harrisii and var. reyi. Accordingly, the palaeoenvironmental conditions inferred indicate that most of the charophyte species were controlled by (i) bathymetry, (ii) clastic content in the sedimentary environment and (iii) salinity. The stratigraphic succession studied shows an upwards increase in clastic content from the base to the top, which is associated with the more humid period recorded along the margins of the Tethys and the Boreal realm during the early Barremian–early late Barremian. In consequence, those species restricted to clastic-poor settings are constrained to the lower part of the section, whereas those taxa that were able to thrive in clastic-rich settings persisted throughout the entire section. This observation establishes a link between the changes observed in the charophyte floras recognized and the environmental changes that occurred during the Barremian in western Europe.
      PubDate: 2022-06-19
       
  • Microfacies and stable isotope analyses (δ13C and δ18O) of the upper
           Serpukhovian-Moscovian carbonates in the Hadim Nappe, southern Turkey: an
           approach to document the Late Paleozoic Ice Age (LPIA)

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      Abstract: Abstract The Late Paleozoic ice age (LPIA) span from latest Devonian to Late Permian (Lopingian) and was one of the three major Phanerozoic glaciations. Large continental ice sheets covered wide parts of Gondwana at high latitudes of the southern hemisphere during the Pennsylvanian and Cisuralian/Early Permian. Many paleoclimate reconstructions have been based on direct evidence of glacial deposits or indirect evidence (far-field effects) of stable isotope proxies and facies analysis of carbonate successions. In this study, we present for the first time Late Mississippian to Middle Pennsylvanian lithostratigraphy, microfacies analysis and stable isotope analyses (δ13C and δ18O) of the stratigraphic units in the Hadim Nappe sections in the Taurides of southern Turkey. Based on detailed sedimentological studies, 12 microfacies and 9 sub-microfacies were defined for this stratigraphic interval. The main microfacies types indicate restricted to open marine, shoal and lagoon or peritidal zones. Evidence from the microfacies and sedimentology, as well as isotope data (δ13C) recovered from the stratigraphic units (Yassıpınar, Gölbelen and Bademli sections) indicate that upper Serpukhovian-Moscovian successions of the Hadim Nappe were indirectly affected by Gondwana glaciation and during the Glacial Period II–III and C3 and C4 of the Australian glacial periods. Late Paleozoic global paleoclimatic changes are recorded in the stable isotope (δ13C and δ18O) record of the studied succession in Tauride Platform in Hadim area and correlate with Russian and Chinese Platforms.
      PubDate: 2022-05-23
      DOI: 10.1007/s10347-022-00649-0
       
  • Multi-technique comparison to assess the effect of bioturbation on
           porosity: a study case for reservoir quality in contourites

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      Abstract: Abstract In recent decades, contourites—as sediments deposited or reworked by bottom currents— have begun to be considered important targets for deep-sea petroleum exploration and exploitation. The incidence of bioturbation, a common feature in contourite deposits, on petrophysical properties has never been approached in detail, however. Here, detailed comparative analysis of the impact of ichnological features on contourite rock properties is initiated through the application of different techniques: (a) X-ray micro-computed tomography (Micro-CT), (b) mercury intrusion porosimetry, and (c) analysis of impregnated thin sections. These three techniques were employed to study two types of contourite deposits, namely clastic (Miocene Morocco) and calcareous ones (Eocene–Miocene Cyprus). The results evidence the suitability of a multi-technique approach. Particular strengths and weaknesses may be encountered for each method depending on the type of material, the ichnological features, and the particular objectives. Trace fossils analysed in calcareous contourites show a neutral effect. In contrast, the burrow lining of Macaronichnus in the clastic contourites has a positive incidence on porosity. The appearance of this ichnotaxa could invigorate the reservoir capacity of bioturbated contourite deposits. Thus, we suggest that detailed analyses must be conducted focusing on ichnological features other than the ones traditionally considered. Still, this is a preliminary effort, and more detailed studies are needed to support the obtained results, and eventually extrapolate them to further contourite deposits.
      PubDate: 2022-05-21
      DOI: 10.1007/s10347-022-00650-7
       
  • The “Orbitolina Limestone” of central Iran: new data about
           microfacies, orbitolinid biostratigraphy, and palaeogeography

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      Abstract: Abstract A section of the Lower Cretaceous Taft Formation of Central Iran, belonging to the Yazd Block yields new data about the microfacies, orbitolinid biostratigraphy, and palaeogeographic setting of this poorly known lithostratigraphic unit. The studied section is characterized throughout by the common occurrence of corals, stromatoporoids and small benthic foraminifera (lenticulinids, Neotrocholina) that indicate deposition in an open marine external carbonate platform environment. The orbitolinid assemblage is characterized by Montseciella' arabica (Henson) in the basal part of the section followed by Rectodictyoconus giganteus Schroeder (up to the top), in association with Paleodictyoconus actinostoma Arnaud-Vanneau & Schroeder, Dictyoconus' pachymarginalis Schroeder, and Palorbitolina ultima Cherchi & Schroeder. The observed ranges of some taxa reveal slight modifications of widely used and, therefore, “standard” orbitolinid biozonations. Like any other group of larger benthic foraminifera, orbitolinids display a facies sensitivity (e.g., inner vs. outer platform) that may lead to different local or regional biozonations evidencing the need for plausibility check of the data when transferred to other regions. Moreover, the orbitolinid assemblages observed from different sections of the Taft Formation give evidence for its diachronous base (late Barremian or early Aptian) becoming younger towards presumably exposed land areas.
      PubDate: 2022-05-11
      DOI: 10.1007/s10347-022-00647-2
       
  • Facies, depositional environments and drowning of Tethyan isolated
           carbonate platforms: the Paleogene carbonates of Malta

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      Abstract: Abstract The < 900-m-thick Paleogene carbonates of the Maltese Islands and offshore wells comprise 16 facies grouped into 7 carbonate facies associations (TA, TB, TC, TD1, TD2, TE1 and TE2). Previous works misclassified facies as belonging to a carbonate ramp, which derailed hydrocarbon exploration. This study confirms that the 200-km-wide, flat-topped, Malta isolated carbonate platform consists of coarse-grained, platform margin sediments surrounding the muddy, shallow marine interior that was tectonically segmented by half graben during foreland extension. Dating by correlation to benthic foraminiferal zones reveals two > 15 Ma-long depositional hiatuses that bound the Eocene carbonates. Cyclic sediments are capped by Eocene gypsum beds and Oligocene palaeosols and were controlled by third-order sea level cycles. About 700 m of inner platform sediments accumulated from the Eocene (TA and TB) to the early Chattian (TC) until an abrupt and ubiquitous change to platform margin facies dominated by coralline red algae and subordinate corals (TD1). The succeeding transgressive rhodalgal biostrome (TD2) aggraded > 40 m and prograded into underfilled half graben, later capped by mobile dunes of large benthic foraminifera (TE1). Deeper water oligophotic to aphotic biota (TE2) draped over the platform by the late Chattian. Increased foreland subsidence and the spread of coarse-grained platform margin sediments signals the beginning of the drowning succession reflecting environmental stress, the decline of coral reef builders, reduced sedimentation rate and increased dispersal rates, culminating in hardgrounds along the drowning surface that terminated carbonate platform sedimentation by the end of the Chattian.
      PubDate: 2022-05-07
      DOI: 10.1007/s10347-022-00648-1
       
  • Sedimentary aspects of the onset of Middle Triassic continental rifting in
           the western end of Neotethys; inferences from the Silica and Torna Nappes,
           NE Hungary: a review

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      Abstract: Abstract The initiation of continental rifting from the latest Early Triassic was reconstructed by correlation of sedimentary formations deposited in the western end of Neotethys (in the Dinaric–Alpine oceanic branch). The shallow-marine and basinal strata of the Silica Nappes and the Bódvarákó Series from the Torna Nappe (located in the southern part of the Inner Western Carpathians) were studied and compared to sedimentary successions described from the Alps, the Carpathians and the Dinarides. The depositional zonation, developed on the shelf during the Late Permian‒Early Triassic transgression, was dissected and rearranged from the latest Early Triassic. The facies pattern and the differential sedimentary evolution of the shelf domains suggest that the accelerated subsidence began in the latest Early Triassic, and was connected to the onset of continental rifting. Three stages are reconstructed in the studied time-frame. (1) Dark grey carbonates, very poor in fossils, were deposited in restricted and hypersaline intraplatform basins in many shelf domains. In the external domains, shallow-marine carbonates, depositional gaps and terrestrial deposits are typical (formations in the Southern Alps, the External Dinarides and the Serbian–Macedonian Massif). From the latest Early Triassic, this latter shelf segment formed a threshold that restricted water circulation from the intraplatform basins. (2) Shallowing-up carbonate successions mark the next stage that implies a period of tectonic quiescence on the shelf from the late Early Anisian to late Middle Anisian. A peculiar change in biota occurring in previously restricted domains was coeval in shallow-marine and deep-marine settings. The biotic change is revealed by observations that dark grey carbonates, which are very poor in fossils, are overlain by carbonate successions rich in fossils typical for normal-marine water. The biota and environmental changes indicate the opening of a passage which allowed the circulation of well-oxygenated and normal-salinity marine water towards the previously restricted depositional areas. The geodynamic setting switching from continental rifting to spreading in the southern sector of the Dinaric–Alpine oceanic branch (Hellenides and Albanides), triggered the opening of the gateway between the future continental margins, i.e., between the External Dinaridic domain (Adria) and Serbian–Macedonian Massif (Eurasia). (3) Following the biotic event in the northern sector of the shelf, subsidence accelerated and additional intraplatform basins opened from the latest Pelsonian.
      PubDate: 2022-04-21
      DOI: 10.1007/s10347-022-00646-3
       
  • Chemical characterisation is rough: the impact of topography and
           measurement parameters on energy-dispersive X-ray spectroscopy in
           biominerals

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      Abstract: Abstract Energy dispersive X-ray microscopy (EDX) is a widely available, inexpensive method of characterizing the in-situ elemental composition of samples in Earth and life sciences. Common protocols and textbooks focussing on material sciences address EDX analysis of metallic samples that can be polished perfectly, whereas geoscientists often investigate specimens with prominent topography and composed of light, difficult to resolve elements. This is further compounded by the scarcity of literature surrounding the methodology of SEM–EDX in the field of palaeontology, leading to common misinterpretations and artefacts during data acquisition. Here, the common errors in elemental composition obtained with EDX arising from surface topography and from parameters subject to user decisions are quantified. As a model, fossil bioapatite (conodonts) and abiotic Durango apatite are used. It is shown that even microscale topography can distort measured composition by up to 34%, whereas topographic features such as tilt with respect to the electron beam lead to differences of up to 85%. Working distance was not the most important parameter affecting the results and led to differences in composition of up to 13%, whereas the choice of standard and its levelling with the sample surface led to inaccuracy reaching 33%. EDX results can be also affected by beam damage and the effects of acceleration voltage on sample acquisition and resolution are quantified. An estimate is provided of the severity of errors associated with samples which cannot satisfy preparation requirements for EDX fully, such as holotypes, and with user decisions. Using a palaeontological example, recommendations are offered for the best parameters and the relative importance of error sources are assessed.
      PubDate: 2022-03-24
      DOI: 10.1007/s10347-022-00645-4
       
  • Evolution of a Miocene canyon and its carbonate fill in the pre-evaporitic
           eastern Mediterranean

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      Abstract: Abstract Extensive canyons, excavated into the margins of the Levant Basin during the Oligocene–Miocene, are interesting case-studies for canyon fills in carbonate settings. The carbonate Pattish Formation, developed along the margins of the pre-evaporitic Messinian Beer Sheva Canyon in Israel, was investigated using both onshore seismic imaging and field data. The canyon has three main seismic facies of fill (1) Subparallel reflections mimicking the canyon´s morphology; (2) chaotic reflections overlying the subparallel ones, and (3) sigmoidal reflections, locally with sharp edges at the canyon margins. The first seismic facies corresponds to the pelagic marls of the Bet Eshel Formation. The other two seismic facies are, respectively, equivalent to bioclastic calcarenite clinobeds with slumps and channels, and to coral–stromatolite reefs and reef slopes of the Pattish Formation observed at outcrop. There were three phases of canyon development: (1) slope incision and headward erosion due to tectonic uplift and eustatic sea-level fall during the Early Oligocene, and large slope failure during the latest Middle Miocene; (2) platform incision and connection with a fluvial system in the Late Miocene related to falling sea level and tectonic uplift; and (3) canyon filling first by pelagic marls at the centre of the canyon, followed by calcarenite clinobeds at the canyon flanks formed by gravity flows. Finally, carbonate production at the margins of the canyon resulted in reefs and associated slopes prograding towards the canyon axis. The late canyon filling phase ended with the deposition of evaporites during the Messinian Salinity Crisis.
      PubDate: 2022-03-23
      DOI: 10.1007/s10347-022-00644-5
       
  • The Jurassic–Cretaceous transition in deep- and shallow-water carbonate
           depositional settings: a case study from the easternmost Getic Carbonate
           Platform (Southern Carpathians, Romania)

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      Abstract: Abstract The Postăvaru Massif is located in the easternmost part of the Getic Carbonate Platform from the Southern Carpathians. The described sections are unevenly distributed in all four tectonic compartments of the Postăvaru Massif (Brașov, Cristian, Râșnov and Postăvaru). Eighteen sections were studied to highlight the biostratigraphic and facies evolution of the Upper Jurassic–Lower Cretaceous (Kimmeridgian–upper Berriasian) transition. Ten facies associations (FA 1–10) were described and they indicate a general shallowing upward tendency, from slope to platform-margin and inner-platform depositional settings. In other cases, the vertical facies stacking patterns indicate a general deepening-upward tendency, at the Upper Jurassic–Lower Cretaceous transition. The micropaleontological assemblage consists of encrusting organisms, dasycladalean algae, foraminifera and pelagic microfossils (calpionellids). As a general rule, this assemblage characterizes four main intervals and stages: Kimmeridgian–upper Tithonian, lower Berriasian, upper Tithonian–Berriasian and upper Berriasian. The carbonate succession from the Postăvaru Massif shares similar characteristics with other parts of the Getic Carbonate Platform (Cioclovina-Bănița area, Buila-Vânturarița Massif, Piatra Craiului-Dâmbovicioara Zone, Western part of Bucegi Massif). Finally, the presence of Lower Cretaceous (Berriasian) deposits is well documented by interpreting various assemblages of microfossils. This study combines microfacies and biostratigraphic analysis techniques to decipher the interplay between environmental conditions, facies distribution and biostratigraphic evolution at the Upper Jurassic–Lower Cretaceous transition, in the easternmost GCP. The Tithonian–Berriasian transition is marked by a continuity of sedimentation, in shallow and deep water depositional environments.
      PubDate: 2022-03-09
      DOI: 10.1007/s10347-022-00643-6
       
  • Ichnology of Lower Cretaceous prodelta and delta front deposits of the
           Sidi Khalif Formation, Central Tunisia

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      Abstract: Abstract This paper describes the ichnology and sedimentology of the middle Berriasian sedimentary succession of the Sidi Khalif Formation outcropping in Jebel Meloussi, Central Tunisia. The succession records deltaic progradation above outer shelf deposits and shows the vertical stacking of thickening and coarsening-upward parasequences dominated by hummocky cross-stratification, parallel lamination and abundant gutter casts. The mudstones and the thinly bedded fine-grained sandstones of the prodelta are characterized by scarce and low diverse horizontal trace fossils of the impoverished distal Cruziana ichnofacies, including cf. Thalassinoides, Phycosiphon, Planolites, Helminthoidichnites and cf. Helminthoidichnites. In contrast, trace fossils of the wave-dominated delta-front are dominated by deposit-feeding ichnotaxa, such as Rhizocorallium commune, Arenicolites isp., R. 'jenense, Thalassinoides and Planolites, which represent the proximal Cruziana ichnofacies. The lack of bioturbation structures in the amalgamated hummocky cross-stratification beds of the delta front is mostly related to the high frequency and/or high intensity episodic erosional amalgamation and deposition associated with storms. The difference between Rhizocorallium ichnospecies help to depict the erosional discontinuities bounding parasequences. The transgressive surfaces (TS) are characterized by R. 'jenense and by R. commune.
      PubDate: 2022-01-04
      DOI: 10.1007/s10347-021-00642-z
       
  • Microbial mats and evaporite facies variation in a supralittoral,
           ephemeral lake, Red Sea coast, Saudi Arabia

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      Abstract: Abstract This study documents the deposits of an ephemeral, shallow lake that is recharged mainly from floods and torrential rainfalls from the Red Sea Mountains, in addition to seawater seepage at its western margin. The lake is desiccated in the summer months into several smaller, ephemeral pans and sabkhas due to excessive evaporation of its waters and decreased inflow of seawater seepage accompanied by the lowered hydraulic gradient between the Red Sea and the lake floor. The formation and distribution of microbial mats, gypsum and halite are discussed with respect to water supply and salinity. Microbial mats dominate the floor of the wintertime lake, and in the summertime, coastal pans where salinity is less than 126%. Gypsum crystals encrust microbial mats at salinities in excess of 182%. The central and eastern pans are floored with halite crusts at a salinity > 250% that develop into tepee polygons through desiccation. The slightly higher topographic sabkha areas around these pans contain subsurface, displacive, lenticular and tabular gypsum crystals, and clear, mosaic halite cement. Most of the water supplied to the supralittoral lake is during the wintertime, from episodic floods from the hinterland with a general increase in salinity towards the sea. However, the pattern of distribution and abundance of microbial mats-gypsum-halite facies are in a reverse order to the direction of water supply and increases in salinity. This ambiguity can be explained by the intermittent supply of seawater seepage from the Red Sea through an artificial barrier that is controlled by tidal range and fluctuations of sea level.
      PubDate: 2021-12-18
      DOI: 10.1007/s10347-021-00641-0
       
  • Changing depositional environments in the semi-restricted Late Jurassic
           Lemeš Basin (Outer Dinarides; Croatia)

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      Abstract: Abstract The up to 450 m-thick Upper Jurassic Lemeš Formation includes organic-rich deep-water (max. ~ 300 m) sedimentary rocks deposited in the Lemeš Basin within the Adriatic Carbonate Platform (AdCP). The Lemeš Formation was investigated regarding (1) bio- and chemostratigraphy, (2) depositional environment, and (3) source rock potential. A multi-proxy approach—microfacies, Rock–Eval pyrolysis, maceral analysis, biomarkers, and stable isotope ratios—was used. Based on the results, the Lemeš Formation is subdivided from base to top into Lemeš Units 1–3. Deposition of deep-water sediments was related to a late Oxfordian deepening event causing open-marine conditions and accumulation of radiolarian-rich wackestones (Unit 1). Unit 2, which is about 50 m thick and Lower early Kimmeridgian (E. bimammatum to S. platynota, ammonite zones) in age, was deposited in a restricted, strongly oxygen-depleted basin. It consists of radiolarian pack- and grainstones with high amounts of kerogen type II-S organic matter (avg. TOC 3.57 wt.%). Although the biomass is predominantly marine algal and bacterial in origin, minor terrestrial organic matter that was transported from nearby land areas is also present. The overlying Unit 3 records a shallowing of the basin and a return to oxygenated conditions. The evolution of the Lemeš Basin is explained by buckling of the AdCP due to ophiolite obduction and compressional tectonics in the Inner Dinarides. Lemeš Unit 2 contains prolific oil-prone source rocks. Though thermally immature at the study location, these rocks could generate about 1.3 t of hydrocarbon per m2 surface area when mature.
      PubDate: 2021-12-18
      DOI: 10.1007/s10347-021-00640-1
       
  • Cyclic nature of the biotic attributes of macroinvertebrate communities in
           the Cenomanian–Turonian strata of Sinai: water depth-driven biological
           responses

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      Abstract: Abstract The analysis of high-resolution stratigraphic data from the Cenomanian–Turonian successions in three sections from Sinai (northeast Egypt) revealed the mechanisms behind water depth-driven biological responses (visible in changes of biodiversity and community structure) of macroinvertebrates. Quantitative biostratigraphical analysis of 127 samples containing 6203 specimens representing 41 genera of molluscs, corals, and echinoids were used to construct changes in the community structure of Cenomanian–Turonian macroinvertebrates. We identified six assemblages that we assigned to two main categories and linked to regional sea-level changes. The first group of assemblages is associated with the initiation of transgression and/or late normal regression, is dominated mainly by opportunistic, epifaunal suspension feeders (oyster bivalves) and is characterized by lower diversity values (low Shannon Index and high dominance). The second category is associated with the maximum flooding zone and dominated by infaunal deposit feeders such as irregular echinoids and by nektonic ammonites and is characterized by higher diversity. The increase in nektonic and decrease in benthic taxa during the latest Cenomanian suggest deepening of the environment. Moreover, the change in the water depth was accompanied by a change in the structure of the macrobenthos.
      PubDate: 2021-11-17
      DOI: 10.1007/s10347-021-00639-8
       
  • Preferential dolomitization in Mio–Pliocene bioclastic clinoforms,
           Bonaire Island, South Caribbean: insights from petrographic and
           geochemical analyses

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      Abstract: Abstract Selective dolomitization, where certain carbonate components are preferentially dolomitized over others, can be significant in the overall dynamic context of the global magnesium cycle. Thus, the abundance of these components can modify the Mg balance between the ocean and sediments, thereby disrupting the Mg cycle in certain geological times. Selective dolomitization may be connected to the apparent correlation between global dolomitization events in the Neogene and the synchronous rise in species abundance of coralline red algae (CRA), but the underlying issue remains unclear. In the Caribbean islands, excellent examples of Neogene partially dolomitized carbonates containing coralline red algal facies are described to understand selective dolomitization of different components (grains and matrix) by examining the well-preserved outcrop of partially dolomitized Mio–Pliocene carbonates at the Seru Grandi locality on Bonaire Island, in the Caribbean. The degree and timing of selective dolomitization of various carbonate components are assessed using petrographical and geochemical methods. The micrite matrix is dolomitized first, followed by coralline red algal bioclasts, and subsequently all other grains. Dolomite crystals appear to originate from within and immediately around coralline algal fragments, suggesting that dolomite could have initiated from internally sourced Mg of the CRA’s high-magnesium calcite skeleton. Collectively, these observations suggest that selective dolomitization is controlled primarily by reactive surface area of the carbonate components, but it is less clear as to whether there is a dependency on original mineralogy.
      PubDate: 2021-10-08
      DOI: 10.1007/s10347-021-00638-9
       
  • 40Ar/39Ar dating and palaeoenvironments at the boundary of the
           early-late Badenian (Langhian-Serravallian) in the northwest margin of the
           Pannonian basin system

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      Abstract: Abstract The sedimentary fill of the Danube Basin represents the northwestern part of the Central Paratethys Sea. The middle Miocene opening of the basin was associated with volcanic activity. The altered tuff to tuffite layers from the northwest part of the Danube Basin occurs within the NN5 Zone and are accompanied by volcanic sediments with andesite clasts. The biotite 40Ar/39Ar age of 13.23 ± 1.95 Ma from the Trakovice-4 (1401–1406 m) tuff to tuffite layer covers a large time span, and this is caused by the fine grain size and alterations to biotite crystals. Nevertheless, the age range thus obtained agrees with biostratigraphic ranking. Fresh amphiboles from the Madunice-3 (1200–1195 m) volcanic sandstone give a more accurate age of 13.83 ± 0.11 Ma, and date the maximum fall in sea level to the beginning of late Badenian (Serravallian). The comparison of age data obtained from sedimentological, biostratigraphic and ecological analyses documents the following: (1) major deposition and subsidence took place in the Blatné depression during the late Badenian (early Serravallian, 13.82–12.6 Ma); (2) although the beginning of late Badenian stage is marked by the Badenian Salinity Crisis, only siliciclastic deposition is recorded within the Danube Basin; (3) during the entire late Badenian stage, upwelling conditions (estuarine circulation) are linked with diversified microfossil associations and dysoxic periods; (4) Moreover, the 40Ar/39Ar age of 13.83 ± 0.11 Ma supports the employment of Globoturborotalita druryi as an index fossil for the onset of the late Badenian. Thus, the Danube Basin represents a location with a well recognised 13.8 Ma early/late Badenian (Langhian /Serravallian) boundary.
      PubDate: 2021-10-03
      DOI: 10.1007/s10347-021-00637-w
       
  • Calcilobes wangshenghaii n. gen., n. sp., microbial constructor of
           Permian–Triassic boundary microbialites of South China, and its place in
           microbialite classification

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      Abstract: Abstract Permian–Triassic boundary microbialites (PTBMs) that formed directly after the end-Permian extinction in the South China Block are dominated by one structure, a lobate-form calcium carbonate construction that created extensive very thin (ca. 2–20 m thick) framework biostromes in shallow marine environments, effectively occupying the ecological position of the prior pre-extinction Permian reefs and/or associated carbonates. In the field, vertical sections show the microbialite is dendrolite (branched) and thrombolite (clotted), but because thrombolite may include branched portions, its structure is overall best classed as thrombolite. In the field and in polished blocks, the microbial material appears as dark carbonate embedded in lighter-coloured micritic sediment, where details cannot be seen at that scale. In thin section, in contrast to the largely unaltered micritic matrix, the microbial constructor is preferentially partly to completely recrystallised, but commonly passes gradationally over distances of a few mm to better-preserved areas comprising 0.1–0.2 mm diameter uneven blobs of fine-grained calcium carbonate (micrite to microsparite). The lobate architecture comprises branches, layers and clusters of blobs ca. 1–20 mm in size, and includes constructed cavities with geopetal sediments, cements and some deposited small shelly fossils. Individual blobs in the matrix may be fortuitous tangential cross sections through margins of accumulated masses, but if separate, may represent building blocks of the masses. The lobate structure is recognised here as a unique microbial taxon and named Calcilobes wangshenghaii n. gen., n. sp. Calcilobes reflects its calcium carbonate composition and lobate form, wangshenghaii for the Chinese geologist (Shenghai Wang) who first detailed this facies in 1994. The structure is interpreted as organically built, and may have begun as separate blobs on the sea floor sediment (that was also composed of micrite but is interpreted as mostly inorganic), by microbial agglutination of micrite. Because of its interpreted original micritic–microsparitic nature, classification as either a calcimicrobe (calcified microbial fossil) or a sedimentary microbial structure is problematic, so C. wangshenghaii has uncertain affinity and nature. Calcilobes superficially resembles Renalcis and Tarthinia, which both form small clusters in shallow marine limestones and have similar problems of classification. Nevertheless, Calcilobes framework architecture contrasts both the open branched geometry of Renalcis, and the small tighter masses of Tarthinia, yet it is more similar to Tarthinia than to Renalcis, and may be a modification of Tarthinia, noting that Tarthinia is known from only the Cambrian. Calcilobes thus joins Renalcis, Tarthinia and also Epiphyton (dendritic form) and others, as problematic microbial structures. Calcilobes has not been recognised elsewhere in the geological record and may be unique to the post-end-Permian extinction facies. C. wangshenghaii occurs almost exclusively in the South China Block, which lay on the eastern margin of Tethys Ocean during Permian–Triassic boundary times; reasons for its absence in western Tethys, except for comparable fabrics in one site in Iran and another in Turkey, are unknown.
      PubDate: 2021-09-27
      DOI: 10.1007/s10347-021-00636-x
       
  • Age, microfacies and depositional environment of the Middle to Late
           Paleocene shallow-marine carbonates in the Sirt Basin of Libya (Upper
           Sabil Formation): “Are Intisar domal structures pinnacle reefs'”

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      Abstract: Abstract In the central-eastern Sirt Basin, enigmatic Intisar domal structures host significant hydrocarbon accumulations. These structures have been commonly interpreted as pinnacle reefs/bioherms occurring in the open-marine basinal environment. Generally, pinnacle reefs/bioherms are mainly characterized by in situ carbonates. The current study challenges the Intisar pinnacle reef/bioherm model by examining one of the domal structures in terms of biostratigraphy, microfacies and depositional environment. These structures were dated using larger benthic foraminifera, which yielded a Middle to Late Paleocene age (Selandian–Early Thanetian). Thirteen microfacies types representing different carbonate ramp environments ranging from outer ramp to inner ramp, were defined. Outer ramp deposits have been observed adjacent to the domal structure, represented mainly by wackestone with small benthic and planktonic foraminifera. The outer ramp deposits are most likely isochronous to the domal structures. The lower part of the domal structures is composed mainly of foraminiferal–algal–echinodermal packstones. The upper part is characterized by foraminiferal–algal–echinodermal packstones with intercalated microbialite–coral boundstones. The euphotic inner ramp deposits are preserved on the crest of the domal structure, consisting of grainstone and packstone rich in Glomalveolina. As a result of this study, the Intisar domal structures are seen as erosional relics of a carbonate ramp and no evidence for pinnacle reef/bioherm model was found.
      PubDate: 2021-08-28
      DOI: 10.1007/s10347-021-00635-y
       
  • Late Aptian carbonate platform evolution and controls (south Tethys,
           Tunisia): response to sea-level oscillations, palaeo-environmental changes
           and climate

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      Abstract: Abstract The late Aptian Lower Serdj Formation (LSF) in the Northern Atlas of Tunisia records a mixed carbonate–siliciclastic system from the southern margin of Tethys. Sedimentological investigations of key sections in the Serdj-Bargou area along a NE–SW-platform-to-basin profile reveal five shallow-marine carbonate units (Cu1, Cu2, Cu3, Cu4a and Cu4b), dominated by subtidal deposits, separated by four terrigenous units (T1, T2, T3, T3a). Twelve basic facies are grouped into six facies associations or zones (FZA to FZF), representing particular palaeo-environments from proximal to distal settings. Carbonate units Cu1, Cu2 and Cu4a are dominated by coral algal-Orbitolina facies representative of a homoclinal ramp. However, units Cu3 and Cu4b are dominated by high-energy oolitic facies of a shoaled ramp. The terrigenous deposits (T1 to T4) are dominated by siliciclastics with shale, sandstone/siltstone and marl and have mostly been assigned to off-platform to basinal environments (FZF). The vertical facies changes are closely related to amplitudes of sea-level fluctuations and late Aptian Tethyan climatic perturbations. The terrigenous units were the result of short cooling periods and a humid climate. Moreover, this climate favoured the development of tide-influenced oolitic shoals, with the nuclei of ooids formed by fine quartz grains. Both the oolitic and siliciclastic deposits reflect episodes of maximum platform progradation basin-ward at a time of low accommodation space through the late Aptian period. Overall the new stratigraphic dataset from the southern Tethys margin is interpreted as reflecting the global Late Aptian cooling episode and sea-level lowstand.
      PubDate: 2021-08-16
      DOI: 10.1007/s10347-021-00634-z
       
 
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