ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Keywords
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Sheward, Rosie M; Poulton, Alex J; Gibbs, Samantha J; Daniels, Chris J; Bown, Paul R (2017): Physiology regulates the relationship between coccosphere geometry and growth phase in coccolithophores. Biogeosciences, 14(6), 1493-1509, https://doi.org/10.5194/bg-14-1493-2017
    Publication Date: 2023-02-13
    Description: Coccolithophores are an abundant phytoplankton group that exhibit remarkable diversity in their biology, ecology and calcitic exoskeletons (coccospheres). Their extensive fossil record is a testament to their important biogeochemical role and is a valuable archive of biotic responses to environmental change stretching back over 200 million years. However, to realise the full potential of this archive for (palaeo-)biology and biogeochemistry requires an understanding of the physiological processes that underpin coccosphere architecture. Using culturing experiments on four modern coccolithophore species (Calcidiscus leptoporus, Calcidiscus quadriperforatus, Helicosphaera carteri and Coccolithus braarudii) from three long-lived families, we investigate how coccosphere architecture responds to shifts from exponential (rapid cell division) to stationary (slowed cell division) growth phases as cell physiology reacts to nutrient depletion. These experiments reveal statistical differences in coccosphere size and the number of coccoliths per cell between these two growth phases, specifically that cells in exponential-phase growth are typically smaller with fewer coccoliths, whereas cells experiencing growth-limiting nutrient depletion have larger coccosphere sizes and greater numbers of coccoliths per cell. Although the exact numbers are species-specific, these growth-phase shifts in coccosphere geometry demonstrate that the core physiological responses of cells to nutrient depletion result in increased coccosphere sizes and coccoliths per cell across four different coccolithophore families (Calcidiscaceae, Coccolithaceae, Isochrysidaceae and Helicosphaeraceae), a representative diversity of this phytoplankton group. Building on this, the direct comparison of coccosphere geometries in modern and fossil coccolithophores enables a proxy for growth phase to be developed that can be used to investigate growth responses to environmental change throughout their long evolutionary history. Our data also show that changes in growth rate and coccoliths per cell associated with growth-phase shifts can substantially alter cellular calcite production. Coccosphere geometry is therefore a valuable tool for accessing growth information in the fossil record, providing unprecedented insights into the response of species to environmental change and the potential biogeochemical consequences.
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 350.8 kBytes
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-11-25
    Description: Coccolithophores are globally important marine calcifying phytoplankton. They contribute to the organic carbon pump through the primary production and the ballast of organic matter, and to the carbonate pump through the production of calcium carbonate. Here we compiled all available scanning electron microscopy (SEM) coccolithophore abundance observations. Taxa were standardized following NannoTax3 to a species level where possible. Subspecies (e.a. C. leptoporus subsp. leptoporus and C. leptoporus subsp. quadriperforatus) were grouped as single species. The database contains 2556 abundance observations from 35 different publications. The data span the period of 1993-2017, with observations from all ocean basins and all seasons, and at depths ranging from the surface to 5000 m. We limited our compilation to SEM observations (or observations which further identified samples with SEM) because SEM provides greater detail of coccolithophore diversity than more commonly used polarized light microscopy. Although this limits the number of observations, this allows for a more in-depth analysis of coccolithophore ecology, such as the ecological significance of the coccolithophore life cycle.
    Keywords: Acanthoica acanthifera; Acanthoica acanthos; Acanthoica biscayensis; Acanthoica maxima; Acanthoica quattrospina; Acanthoica spp.; Algirosphaera cucullata; Algirosphaera robusta; Algirosphaera spp.; Alisphaera capulata; Alisphaera extenta; Alisphaera gaudii; Alisphaera ordinata; Alisphaera pinnigera; Alisphaera quadrilatera; Alisphaera spp.; Alisphaera unicornis; Anthosphaera lafourcadii; Anthosphaera periperforata; Anthosphaera spp.; Balaniger virgulosa; Braarudosphaera bigelowii; Calcidiscus leptoporus; Calcidiscus spp.; Calciopappus caudatus; Calciopappus spp.; Calciosolenia brasiliensis; Calciosoleniaceae spp.; Calciosolenia murrayi; Calciosolenia spp.; Calicasphaera blokii; Calicasphaera concava; Calicasphaera diconstricta; Calyptrolithina multipora; Calyptrosphaera cialdii; Calyptrosphaera dentata; Calyptrosphaera heimdalae; Calyptrosphaera sphaeroidea; Canistrolithus spp.; Canistrolithus valliformis; Ceratolithus cristatus; Ceratolithus spp.; Chrysotila carterae; Chrysotila roscoffensis; Coccoliths, other; Coccolithus pelagicus; Corisphaera gracilis; Corisphaera spp.; Corisphaera tyrrheniensis; Coronosphaera maxima; Coronosphaera mediterranea; Coronosphaera spp.; Cyrtosphaera aculeata; Cyrtosphaera cidaris; Cyrtosphaera spp.; DATE/TIME; DEPTH, water; Discosphaera tubifera; Emiliania huxleyi; Ericiolus sp.; Florisphaera profunda; Flosculosphaera calceolariopsis; Formonsella pyramidosa; Gephyrocapsa ericsonii; Gephyrocapsa muellerae; Gephyrocapsa oceanica; Gephyrocapsa ornata; Gephyrocapsa spp.; Gladiolithus flabellatus; Gliscolithus amitakareniae; Hayaster perplexus; Helicosphaera carteri; Helicosphaera cornifera; Helicosphaera hyalina; Helicosphaera pavimentum; Helicosphaera spp.; Helicosphaera wallichii; Helladosphaera cornifera; Helladosphaera pienaarii; Helladosphaera vavilovii; Heterococcolithophores; Holococcolithophora kastriensis; Holococcolithophore spp.; Homozygosphaera spinosa; Homozygosphaera spp.; Homozygosphaera triarcha; Homozygosphaera vercelli; Hughesius youngii; Hymenomonas lacuna; Hymenomonas roseola; Hymenomonas spp.; Jomonlithus spp.; LATITUDE; LONGITUDE; Michaelsarsia adriaticus; Michaelsarsia elegans; Michaelsarsia spp.; Ochrosphaera neapolitana; Oolithotus antillarum; Oolithotus fragilis; Oolithotus spp.; Ophiaster formosus; Ophiaster hydroideus; Ophiaster minimus; Ophiaster reductus; Ophiaster spp.; Palusphaera sp.; Palusphaera spp.; Palusphaera vandelii; Pappomonas borealis; Pappomonas flabellifera; Pappomonas sp.; Pappomonas spp.; Papposphaera arctica; Papposphaera lepida; Papposphaera sagittifera; Papposphaera sp.; Papposphaera spp.; Papposphaera thomsenii; Picarola margalefii; Placorhombus ziveriae; Polycrater sp.; Polycrater spp.; Pontosphaera discopora; Pontosphaera japonica; Pontosphaera multipora; Pontosphaera spp.; Pontosphaera syracusana; Poricalyptra aurisinae; Poricalyptra isselii; Poricalyptra magnaghii; Poritectolithus maximus; Poritectolithus poritectum; Pseudowigwamma scenozonion; Reference/source; Reticulofenestra parvula; Reticulofenestra sessilis; Reticulofenestra spp.; Rhabdosphaera clavigera; Rhabdosphaera spp.; Rhabdosphaera xiphos; Sample method; Scyphosphaera apsteinii; Scyphosphaera spp.; see sample method; Solisphaera helianthiformis; Solisphaera spp.; Sphaerocalyptra adenensis; Sphaerocalyptra dermitzakii; Sphaerocalyptra quadridentata; Sphaerocalyptra sp.; Sphaerocalyptra spp.; Syracolithus bicorium; Syracolithus quadriperforatus; Syracolithus schilleri; Syracolithus sp.; Syracolithus spp.; Syracosphaera amoena; Syracosphaera ampliora; Syracosphaera anthos; Syracosphaera arethusae; Syracosphaera bannockii; Syracosphaera borealis; Syracosphaera castellata; Syracosphaera corolla; Syracosphaera delicata; Syracosphaera dilatata; Syracosphaera epigrosa; Syracosphaera exigua; Syracosphaera florida; Syracosphaera gaarderae; Syracosphaera halldalii; Syracosphaera hastata; Syracosphaera histrica; Syracosphaera lamina; Syracosphaera leptolepis; Syracosphaera marginiporata; Syracosphaera molischii; Syracosphaera nana; Syracosphaera nodosa; Syracosphaera noroitica; Syracosphaera orbiculus; Syracosphaera ossa; Syracosphaera prolongata; Syracosphaera protrudens; Syracosphaera pulchra; Syracosphaera reniformis; Syracosphaera rotula; Syracosphaera sp.; Syracosphaera spp.; Syracosphaera squamosa; Syracosphaera strigilis; Syracosphaera tumularis; Tergestiella adriatica; Tetralithoides quadrilaminata; Turrilithus latericioides; Turrisphaera spp.; Umbellosphaera irregularis; Umbellosphaera spp.; Umbellosphaera tenuis; Umbilicosphaera anulus; Umbilicosphaera foliosa; Umbilicosphaera hulburtiana; Umbilicosphaera sibogae; Umbilicosphaera spp.; Wigwamma antarctica; Wigwamma spp.; Wigwamma triradiata; Zygosphaera amoena; Zygosphaera marsilii
    Type: Dataset
    Format: text/tab-separated-values, 685008 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-01-26
    Description: Coccolithophores, a diverse group of phytoplankton, make important contributions to pelagic calcite production and export, yet the comparative biogeochemical role of species other than the ubiquitous Emiliania huxleyi is poorly understood. Here we examined the relative importance of E. huxleyi and two Coccolithus species (Coccolithus pelagicus and Coccolithus braarudii), in terms of daily calcite production, by culturing E. huxleyi and Coccolithus in parallel, and comparing growth rates and biometrically determined cellular carbon calcite quotas. Biometric measurements of Coccolithus species, and E. huxleyi cell diameters, were performed using polarised light microscopy. Scanning electron microscopy was used for all other biometric measurements of E. huxleyi.
    Keywords: Cell, diameter; Coccoliths per coccosphere; Coccosphere, diameter; Coccosphere, length; Experiment; Growth rate; Number; Species; Strain; Treatment: daily irradiance; Treatment: light:dark cycle; Treatment: temperature
    Type: Dataset
    Format: text/tab-separated-values, 10998 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Daniels, Chris J; Poulton, Alex J; Esposito, Mario; Paulsen, Maria Lund; Bellerby, Richard G J; St John, M; Martin, Adrian Peter (2015): Phytoplankton dynamics in contrasting early stage North Atlantic spring blooms: composition, succession, and potential drivers. Biogeosciences, 12(8), 2395-2409, https://doi.org/10.5194/bg-12-2395-2015
    Publication Date: 2024-02-02
    Description: The Deep Convection cruise repeatedly sampled two locations in the North Atlantic, sited in the Iceland and Norwegian Basins, onboard the RV Meteor (19 March - 2 May 2012). Samples were collected from multiple casts of a conductivity-temperature-depth (CTD) - Niskin rosette at each station. Water samples for primary production rates, community structure, chlorophyll a [Chl a], calcite [PIC], particulate organic carbon [POC] and biogenic silicic acid [BSi] were collected from predawn casts from six light depths (55%, 20%, 14%, 7%, 5% and 1% of incident PAR). Additional samples for community structure and ancillary parameters were collected from a second cast. Carbon fixation rates were determined using the 13C stable isotope method. Water samples for diatom and micro zooplankton counts, collected from the predawn casts, were preserved with acidic Lugol's solution (2% final solution) and counted using an inverted light microscope. Water samples for coccolithophore counts were collected onto cellulose nitrate filters and counted using polarising light microscopy. Water samples for Chl a analysis were filtered onto MF300 and polycarbonate filters and extracted in 90% acetone. PIC and BSi samples were filtered onto polycarbonate filters and analysed using an inductively coupled plasma emission optical spectrometer and a SEAL QuAAtro autoanalyser respectively.
    Keywords: Basin Scale Analysis, Synthesis and Integration; Biogenic silica; Bottle number; Carbon, inorganic, particulate; Carbon, organic, particulate; Chaetoceros spp.; Chlorophyll a as carbon; Ciliates; Coccolithus leptoporus; Coccolithus pelagicus; Coronosphaera mediterranea; Counting; Cryptophytes; CTD/Rosette; CTD-RO; Cylindrotheca spp.; Dactyliosolen spp.; Date/Time of event; Deep Convection Cruise; DEPTH, water; Diatoms, centrales indeterminata; Diatoms, pennales indeterminata; Dinoflagellates, armoured; Emiliania huxleyi; EURO-BASIN; Event label; Guinardia striata; Gymnodinium spp.; Gyrodinium spp.; Latitude of event; Leptocylindrus spp.; Longitude of event; M87/1_413-1; M87/1_421-1; M87/1_447-1; M87/1_460-1; M87/1_516-1; M87/1_532-1; M87/1_553-1; M87/1_572-1; M87/1_614-1; M87/1_618-1; M87/1_641-1; M87/1_667-1; M87/1_672-1; M87/1_689-1; M87/1a; M87/1b; Meteor (1986); Navicula spp.; Primary production, carbon assimilation (24 hr.); Pseudo-nitzschia spp.; Rhizosolenia spp.; Silicoflagellates; Station 1; Station 2; Syracosphaera pulchra; Thalassionema spp.; Thalassiosira spp.
    Type: Dataset
    Format: text/tab-separated-values, 832 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Smith, Helen Elizabeth Katie; Tyrrell, Toby; Charalampopoulou, Anastasia; Dumousseaud, Cynthia; Legge, Oliver J; Birchenough, Sarah; Pettit, Laura Rachel; Garley, Rebecca; Hartman, Sue E; Hartman, Mark C; Sagoo, Navjit; Daniels, Chris J; Achterberg, Eric Pieter; Hydes, D J (2012): Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay. Proceedings of the National Academy of Sciences, 109(23), 8845-8849, https://doi.org/10.1073/pnas.1117508109
    Publication Date: 2024-03-15
    Description: Coccolithophores are an important component of the Earth system, and, as calcifiers, their possible susceptibility to ocean acidification is of major concern. Laboratory studies at enhanced pCO2 levels have produced divergent results without overall consensus. However, it has been predicted from these studies that, although calcification may not be depressed in all species, acidification will produce "a transition in dominance from more to less heavily calcified coccolithophores" [Ridgwell A, et al., (2009) Biogeosciences 6:2611-2623]. A recent observational study [Beaufort L, et al., (2011) Nature 476:80-83] also suggested that coccolithophores are less calcified in more acidic conditions. We present the results of a large observational study of coccolithophore morphology in the Bay of Biscay. Samples were collected once a month for over a year, along a 1,000-km-long transect. Our data clearly show that there is a pronounced seasonality in the morphotypes of Emiliania huxleyi, the most abundant coccolithophore species. Whereas pH and CaCO3 saturation are lowest in winter, the E. huxleyi population shifts from 〈10% (summer) to 〉90% (winter) of the heavily calcified form. However, it is unlikely that the shifts in carbonate chemistry alone caused the morphotype shift. Our finding that the most heavily calcified morphotype dominates when conditions are most acidic is contrary to the earlier predictions and raises further questions about the fate of coccolithophores in a high-CO2 world.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cell density; Cell density, standard error; Chromista; Coast and continental shelf; Coccoliths, overcalcified; Confidence interval; Coulometric titration; Counting; DATE/TIME; Emiliania huxleyi; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Haptophyta; LATITUDE; LONGITUDE; North Atlantic; Number of measurements; OA-ICC; Ocean Acidification International Coordination Centre; Open ocean; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate; Phytoplankton; Potentiometric titration; Salinity; Silicate; Single species; Species; Temperate; Temperature, water; Volume
    Type: Dataset
    Format: text/tab-separated-values, 13730 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2024-03-14
    Keywords: Calcium carbonate production of carbon; Calcium carbonate production of carbon, standard deviation; Coccolithophoridae, total; Cruise/expedition; DATE/TIME; DEPTH, water; Emiliania huxleyi; Incubation duration; LATITUDE; LONGITUDE; Method comment; Ocean and sea region; Percentage; Primary production of carbon; Primary production of carbon, standard deviation; Principal investigator; Reference/source; Station label; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 35037 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
  • 8
    Publication Date: 2018-02-01
    Print ISSN: 0304-4203
    Electronic ISSN: 1872-7581
    Topics: Geosciences
    Published by Elsevier
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2017-03-24
    Description: Coccolithophores are an abundant phytoplankton group that exhibit remarkable diversity in their biology, ecology and calcitic exoskeletons (coccospheres). Their extensive fossil record is a testament to their important biogeochemical role and is a valuable archive of biotic responses to environmental change stretching back over 200 million years. However, to realise the full potential of this archive for (palaeo-)biology and biogeochemistry requires an understanding of the physiological processes that underpin coccosphere architecture. Using culturing experiments on four modern coccolithophore species (Calcidiscus leptoporus, Calcidiscus quadriperforatus, Helicosphaera carteri and Coccolithus braarudii) from three long-lived families, we investigate how coccosphere architecture responds to shifts from exponential (rapid cell division) to stationary (slowed cell division) growth phases as cell physiology reacts to nutrient depletion. These experiments reveal statistical differences in coccosphere size and the number of coccoliths per cell between these two growth phases, specifically that cells in exponential-phase growth are typically smaller with fewer coccoliths, whereas cells experiencing growth-limiting nutrient depletion have larger coccosphere sizes and greater numbers of coccoliths per cell. Although the exact numbers are species-specific, these growth-phase shifts in coccosphere geometry demonstrate that the core physiological responses of cells to nutrient depletion result in increased coccosphere sizes and coccoliths per cell across four different coccolithophore families (Calcidiscaceae, Coccolithaceae, Isochrysidaceae and Helicosphaeraceae), a representative diversity of this phytoplankton group. Building on this, the direct comparison of coccosphere geometries in modern and fossil coccolithophores enables a proxy for growth phase to be developed that can be used to investigate growth responses to environmental change throughout their long evolutionary history. Our data also show that changes in growth rate and coccoliths per cell associated with growth-phase shifts can substantially alter cellular calcite production. Coccosphere geometry is therefore a valuable tool for accessing growth information in the fossil record, providing unprecedented insights into the response of species to environmental change and the potential biogeochemical consequences.
    Print ISSN: 1726-4170
    Electronic ISSN: 1726-4189
    Topics: Biology , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2016-10-13
    Electronic ISSN: 1932-6203
    Topics: Medicine , Natural Sciences in General
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...