Planktonic Organisms (planktonic + organism)

Distribution by Scientific Domains


Selected Abstracts


Increase in photosynthetic efficiency as a strategy of planktonic organisms exploiting deep lake layers

FRESHWATER BIOLOGY, Issue 2 2004
Beatriz Modenutti
Summary 1. The photosynthetic efficiencies of the mixotrophic ciliate Ophrydium naumanni and the autotrophic dinoflagellate Gymnodinium paradoxum were investigated using laboratory and field experiments in Lake Moreno Oeste (41°5,S and 71°33,W, 758 m a.s.l.), in the Nahuel Huapi System (North Patagonia, Argentina). 2. The effect of different underwater light intensities on net primary production (NPP) was assessed during one summer. Additionally, laboratory experiments were carried out to obtain photosynthesis-irradiance response curves for each species. 3. Ophrydium naumanni and G. paradoxum dominated the metalimnetic (30 m depth) deep chlorophyll maximum (DCM) in the lake. 4. Despite these deep higher abundances, the cell-specific production of both species was higher at 10 m than at 30 m (DCM) depth. In addition, at 5 m depth, NPP was reduced by PAR + UV-A radiation. 5. Both species exhibited a positive NPP at very low irradiance but the mixotrophic ciliate was more efficient in exploiting the DCM irradiance level both in situ and at comparable light intensities in laboratory experiments. Light acclimatised O. naumanni showed a higher NPP at lower irradiances and photoinhibition at medium and high irradiances. 6. Under the strong wind-driven turbulence commonly found in Patagonian lakes, organisms cannot select their position in the epilimnetic water column and will be dragged to potentially harmful UV radiation levels. Thus, metalimnetic DCM colonisation by these two species represents a tradeoff between higher survival and lower cell-specific NPP. [source]


Latitudinal gradient of taxonomic richness: combined outcome of temperature and geographic mid-domains effects?

JOURNAL OF ZOOLOGICAL SYSTEMATICS AND EVOLUTIONARY RESEARCH, Issue 3 2005
A. Brayard
Abstract For several decades, the origin and ecological consequences of large-scale continental and marine Latitudinal Gradients of Taxonomic Richness (LGTR) have been intensively debated. Among the various hypotheses, it has been proposed that a LGTR is the by-product of a geographic mid-domain effect, i.e. the result of a random distribution of ranges of taxa between physical hard boundaries such as the continent/ocean interface. In order to more realistically evaluate the role of the mid-domain effect on the origin and evolution of the LGTR of marine planktonic organisms, we present a 2D model based on a cellular-automaton approach in which sea surface temperatures (SST) and currents are forced in the biogeographic dispersal of a randomly generated clade (a 2D ,geophyletic' model). Sensitivity experiments allow to evaluate the effects of currents, SST and the geographical origin of a clade on the formation and shape of a LGTR for planktonic organisms when coupled with a geographic mid-domain effect. Results are discussed in the light of the empirical LGTR of extant planktonic Foraminifera in the Atlantic Ocean. Independently of any other biotic or abiotic parameter, inclusive of the surface currents and origination/extinction absolute and relative rates, our simulations show that the coupling of the mid-domain effect with two critical parameters, namely the shape and intensity of the SST gradient and the geographic origin of a clade, produces realistic patterns of diversity when compared with the observed LGTR of extant atlantic planktonic foraminifera. The results illustrate a non-linear relation between a unimodal latitudinal SST gradient and a resulting bimodal LGTR characterized by a drop in species richness near the equator. This relation indicates that the SST gradient exerts a mid-domain effect on the LGTR. The latitudinal positions of the modal values of the LGTR are also found to be influenced by the geographic origin of the simulated clade. Résumé Depuis plusieurs décennies, l'origine et l'interprétation écologique des Gradients Latitudinaux de Richesse Taxonomique (LGTR) marins ou continentaux, ont été intensivement débattues. Parmi de nombreuses hypothèses, il a été proposé qu'un LGTR puisse être le sous-produit d'un effet de milieu de domaine géographique, i.e. le résultat d'une distribution aléatoire des répartitions des taxa entre deux limites physiques telles que l'interface continent/océan. Afin d'évaluer plus efficacement le rôle de cet effet sur l'origine et l'évolution des LGTR des organismes planctoniques marins, nous proposons un modèle 2D basé sur une approche de type automate cellulaire dans laquelle les températures des eaux de surface (SST) et les courants régulent la dispersion biogéographique d'une phylogénie générée aléatoirement (un modèle «géophylétique»). Ce modèle permet d'évaluer les effets des courants, des SST et de la dépendance thermique des espèces sur la mise en place et la forme d'un LGTR impliquant des organismes planctoniques. Il permet aussi de discuter des influences respectives de ces paramètres quand ils sont superposés à l'effet de milieu de domaine géographique. Les résultats sont discutés à partir du LGTR empirique des foraminifères planctoniques atlantiques actuels. Indépendamment de tout autre paramètre biotique ou abiotique, y compris les courants ainsi que les taux relatifs et absolus d'apparition et d'extinction, les simulations font apparaître que le couplage de l'effet de milieu de domaine à deux contraintes principales, la forme et l'intensité du gradient de SST ainsi que la localisation géographique de l'origine du clade, produit des représentations réalistes de la diversité comparées au LGTR observé pour les foraminifères planctoniques actuels de l'océan atlantique. Nos résultats indiquent une relation non-linéaire entre la structure globale d'un gradient unimodal de SST et le LGTR bimodal correspondant, montrant une baisse de richesse spécifique au niveau de l'équateur. Cette relation suggère que le gradient de SST exerce un effet de milieu de domaine thermique sur le LGTR. Les positions latitudinales des modes du LGTR sont aussi influencées par le lieu d'origine du clade simulé. [source]


Biotic diachroneity during the Ordovician Radiation: evidence from South China

LETHAIA, Issue 3 2006
Renbin Zhan
The Ordovician radiation was one of the most marked and sustained increases in Phanerozoic biodiversification; nevertheless it occurred against a background of minimal global climatic and environmental perturbations. Detailed investigations of the Ordovician successions on the Yangtze Platform of the South China palaeoplate indicate that: (1) the brachiopod ,- and ,-diversity changes are diachronous; (2) macroevolutionary patterns were different across the South China palaeoplate, with the Early Ordovician brachiopod radiation first occurring in normal marine, shallow-water environments and then moving gradually to both nearer-shore and offshore locations; (3) the main contributors to the initial Ordovician brachiopod radiation were the Orthida and Pentamerida; the typical Ordovician brachiopod fauna, dominated by the Orthida and Strophomenida, did not appear until the late Mid Ordovician (Undulograptus austrodentatus Biozone) when the Strophomenida apparently replaced the dominant position of the Pentamerida within the fauna; (4) different ecotypes (e.g., sessile benthos, mobile benthos together with pelagic and planktonic organisms) demonstrate substantially different macroevolutionary patterns. The Ordovician brachiopod radiation of South China was apparently earlier than that suggested by global trends together with the data available from other palaeoplates or terranes, which may be related to its unique palaeogeographic position (peri-Gondwanan terrane gradually moving to equatorial latitudes). [source]