<i>Virgatasporites</i> and <i>Attritasporites</i>: the oldest land plant derived spores, cryptospores or acritarchs?

peer reviewe

The palaeogeographical impact on the biodiversity of marine faunas during the Ordovician radiations

Diversification is a key property of life. Building on John Phillips' (1860) classic, iconic curve, Phanerozoic biodiversity trajectories have been based, subsequently, on the availability of additional and renewed sets of data and increasingly sophisticated analytical methods. Using relatively few single sources of data from global databases, the shapes of recent biodiversity curves for Ordovician biotas have predictably converged promoting acceptance of discrete events, aligned with relatively few peaks and discrete drivers. There has been a resistance to investigate under the curves and examine the many and varied causes of biodiversity. Most of the data available pertains to the most abundant part of the benthos, the brachiopods, and more especially their occurrences in Baltica and Laurentia together with South China. Exploration of several regional datasets, deconstructed from global curves, for some key fossil groups indicates the regions that do have their own distinctive biodiversity signals, usually associated with low-latitude settings, but also highlights significant gaps in our knowledge

Which early Palaeozoic acritarchs might be dinoflagellate cysts?

Small, organic-walled microfossils were usually attributed to the general term ‘hystrichospheres’ until the early 1960’s. After the discovery that many of these ‘hystrichospheres’ displayed morphological characteristics that are specific for dinoflagellates namely having a cingulum, a sulcus, an operculum and a para-tabulation, Evitt (1963) created the new term ‘acritarchs’ to classify all the remaining forms of unknown biological affinity and separate these from dinocysts. The acritarchs therefore include various kinds of organisms that have been affiliated to animal remains, fossil spores of various groups, and to several classes of (green) algae, including the prasinophycean, zygnematophycean or chlorophycean groups, for example. Although of unknown biological affinities by definition, many Palaeozoic acritarchs, in particular taxa from the Ordovician, Silurian and Devonian, have been compared morphologically to dinoflagellates. Such morphotypes have therefore been considered to be the resting cysts of phytoplankton since many years. The diversity of (planktonic) dinocyst-like taxa strongly increases in the late Cambrian, triggering probably the onset of the ‘Ordovician plankton revolution.’ These acritarchs are virtually impossible to differentiate from dinocysts, showing often the same process morphology (see Kröck et al., this conference). Furthermore, their palaeoecological distribution patterns, following inshore-offshore trends, is identical to those of dinoflagellates. Also, their biogeographical distribution is comparable to that of modern dinoflagellate taxa. We consider that some Palaeozoic acritarchs might therefore have been produced by dinoflagellate-like species, although they do not display all morphological criteria necessary to be recognized as a dinoflagellate cyst

Morphological variability of peteinoid acritarchs from the Middle Ordovician of Öland, Sweden, and implications for acritarch classification

Investigation of large populations of peteinoid acritarchs recovered from Middle Ordovician strata of the Hälludden and Horns Udde quarry sections (Öland, Sweden) allows for statistical analyses based on morphometric measurements. The results indicate the presence of assemblages with a continuous variability of morphotypes, thus a distinction of different peteinoid acritarch taxa in the sections proved to be impossible. This challenges the currently accepted classification based on a differentiation into the three genera Peteinosphaeridium, Cycloposphaeridium and Liliosphaeridium, and a multitude of different species; individual taxa are essentially arbitrary as morphotypes intergrade. Investigations on modern dinoflagellates show that these can develop variable cyst morphologies depending on environmental factors. By analogy, it can be hypothesised that the different morphologies observed among the peteinoid acritarchs from Öland are cysts produced by only very few phytoplanktic organisms (or even a single species) with high morphological variability