Seasonality of microzooplankton grazing in the northern Wadden Sea     

Martina Loebl  Justus E.E. Van Beusekom 《Journal of Sea Research》2008,59(4):203-216

A sequence of nine dilution experiments was conducted according to Landry and Hassett [Landry, M.R., Hassett, R.P., 1982. Estimating the grazing impact of marine microzooplankton. Mar. Biol. 67, 283–288] in the northern Wadden Sea from March until October 2004 to investigate the seasonality of microzooplankton grazing. From March until April, no grazing was observed. Microzooplankton grazing started in May (0.66 d^− 1) and increased until August (1.22 d^− 1). In October microzooplankton grazing was low again (0.17 d^− 1). Phytoplankton growth rates varied between 0 and 1.1 d^− 1. Since the reliability of dilution experiments is still frequently discussed in literature, we tested if our data obtained by dilution experiments reflected short-term in situ phytoplankton dynamics of the study site. We scaled experimental growth rates to water column irradiance, calculated short-term chlorophyll-a dynamics and compared the results to in situ measured chlorophyll-a concentrations. Calculated chlorophyll-a concentrations correlated significantly with in situ measured chlorophyll-a concentrations but slightly overestimated the in situ measured chlorophyll-a. This overestimation was in the range of phytoplankton assimilation reported for the Wadden Sea benthos. We will show that microzooplankton grazing had a large impact during the Phaeocystis bloom and during summer suggesting that a large proportion of phytoplankton biomass remained the pelagic food web. Microzooplankton grazing did not impact the diatom spring bloom and its demise.  相似文献   

Aerosol particle chemical characteristics measured from aircraft in the lower troposphere during ACE‐2     

Martina Schmeling  Lynn M. Russell  Carynelisa Erlick  Donald R. Collins  Haflidi Jonsson  Qing Wang  Peter Kregsamer  Christina Streli 《Tellus. Series B, Chemical and physical meteorology》2000,52(2):185-200

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Setting a size-exclusion limit to remove toxic dinoflagellate cysts from ships' ballast water     

Doblin MA  Dobbs FC 《Marine pollution bulletin》2006,52(3):259-263

Dinoflagellate cysts are well-recognized biological constituents of ships' ballast tanks. They are present in ballast water, sediments and residual water in drained tanks, and in biofilms formed on interior tank surfaces. Therefore, cysts have the potential to be released during ballast discharge. The International Maritime Organization's (IMO) Ballast Water Management Convention (promulgated February 2004) stipulates a performance standard (Annex, Regulation D2) requiring discharged ballast water contain <10 viable organisms between 10 and 50 microm per ml and <10 viable organisms 50 microm per m3. The proposed size limit has potential to exclude both the smallest toxic and the largest toxic and non-toxic dinoflagellate (and other microalgal) cysts from discharged ballast water. Despite the appropriateness of size cutoffs however, ballast water containing predominantly small cysts (<50 microm) could be deemed in compliance with the performance standard, even without treatment, while ballast water having the same concentration of larger cysts (>50 microm) could require a multiple-log reduction in abundance before its permissible discharge. Also of concern, it remains uncertain whether ballast-water treatment can remove sufficient organisms, including dinoflagellate cysts, to meet the performance standard.  相似文献   

Spatio-temporal microseismicity clustering in the Cretan region     

Dirk Becker  Thomas Meier  Martina Rische  Marco Bohnhoff  Hans-Peter Harjes 《Tectonophysics》2006,423(1-4):3

Spatio-temporal clustering of microseismicity in the central forearc of the Hellenic Subduction Zone in the area of Crete is investigated. Data for this study were gathered by temporary short period networks which were installed on the islands of Crete and Gavdos between 1996 and 2004. The similarity of waveforms is quantified systematically to identify clusters of microseismicity. Waveform similarities are calculated using an adaptive time window containing both the P- and S-wave onsets. The cluster detection is performed by applying a single linkage approach. Clusters are found in the interplate seismicity as well as in the intraplate seismicity of the continental crust in the region of the transtensional Ptolemy structure. The majority of the clusters are off the southern coast of Crete, in a region of elevated intraplate microseismic activity within the Aegean plate. Clusters in the Gavdos region are located at depths compatible with the plate interface while cluster activity in the region of the Ptolemy trench is distributed along a nearly vertical structure throughout the crust extending down to the plate interface. Most clusters show swarm-like behaviour with seismic activity confined to only a few hours or days, without a dominant earthquake and with a power law distribution of the interevent times.For the largest cluster, precise relocations of the events using travel time differences of P- and S-waves derived from waveform cross correlations reveal migration of the hypocenters. This cluster is located in the region of the Ptolemy trench and migration occurs along the strike of the trench at  500 m/day.Relocated hypocenters as well as subtle differences in the waveforms suggest an offset between the hypocenters and thus the activation of distinct patches on the rupture surface. The observed microseismicity patterns may be related to fluids being transported along the plate interface and escaping towards the surface in zones of crustal weakness (Ptolemy structure), triggering swarm-like cluster activity along its way.  相似文献   

Aptian (Lower Cretaceous) biostratigraphy and cephalopods from north central Tunisia     

Jens Lehmann  Matthias Heldt  Martina Bachmann  Mohamed E. Hedi Negra 《Cretaceous Research》2009,30(4):895-910

Thick Aptian deposits in north central Tunisia comprise hemipelagic lower Aptian, reflecting the sea-level rise of OAE 1a, and an upper Aptian shallow marine environment characterized by the establishment of a carbonate platform facies. Carbon stable isotope data permit recognition of the OAE 1a event in the Djebel Serdj section. Cephalopods are rare throughout these successions, but occurrences are sufficient to date the facies changes and the position of the OAE1a event. Ammonite genera include lower Aptian Deshayesites, Dufrenoyia, Pseudohaploceras, Toxoceratoides and ?Ancyloceras; and upper Aptian Zuercherella, Riedelites and Parahoplites. Correlation of carbon isotope data with those of other Tethyan sections is undertaken together with the integration of planktonic foraminiferal data.  相似文献   

Impact of vegetation variability on potential predictability and skill of EC-Earth simulations     

Martina Weiss  Bart van den Hurk  Reindert Haarsma  Wilco Hazeleger 《Climate Dynamics》2012,39(11):2733-2746

Climate models often use a simplified and static representation of vegetation characteristics to determine fluxes of energy, momentum and water vapour between surface and lower atmosphere. In order to analyse the impact of short term variability in vegetation phenology, we use remotely-sensed leaf area index and albedo products to examine the role of vegetation in the coupled land–atmosphere system. Perfect model experiments are carried out to determine the impact of realistic temporal variability of vegetation on potential predictability of evaporation and temperature, as well as model skill of EC-Earth simulations. The length of the simulation period is hereby limited by the availability of satellite products to 2000–2010. While a realistic representation of vegetation positively influences the simulation of evaporation and its potential predictability, a positive impact on 2?m temperature is of smaller magnitude, regionally confined and more pronounced in climatically extreme years.  相似文献   

The making and unmaking of gendered crops in northern Ghana   总被引：2，自引：0，他引：2  

Martina A. Padmanabhan 《Singapore journal of tropical geography》2007,28(1):57-70

In rural West Africa, the gendered division of labour extends to labelling certain crops as 'male' or 'female'. With the introduction of new varieties of crops and technologies, these constructions of gendered plants undergo a process of renegotiation at social intrafaces. This process of attaching meaning to new features in cultivation results in the remaking of gendered crops. These negotiations, in turn, have an effect on the construction of gender in specific ethnic and environmental settings, unlinking labour from its gendered connotations and, thus, unmaking the social meaning and creating room for manoeuvre. Based on fieldwork among the Dagomba and Kusasi people in northern Ghana, this study examines how gendered responsibilities and access to the cultivation of crops are linked and expressed in obligations related to the cultural ideal of a proper meal, in this case consisting of the food categories (male) staple and (female) soup, which serve as the blueprint for assigning crops to a specific gender.  相似文献   

Ordovician K-bentonites in the upper-plate active margin of Western Gondwana, (Famatina Ranges): Stratigraphic and palaeogeographic significance   总被引：1，自引：0，他引：1  

Ricardo A. Astini  Gilda Collo  Federico Martina   《Gondwana Research》2007,11(3):311-325

Numerous, thin-bedded, tabular pale-yellowish clay bands are interlayered with black shales in a biostratigraphically constrained Early Ordovician volcano-sedimentary succession at Famatina, western Argentina. This region was part of a fairly continuous upper-plate, convergent volcanic chain that fringed western Gondwana. Mineralogy on both clay and non-clay fractions, whole rock chemistry and field observations on these distinctive event-beds indicate that they originated as relatively coarse fallout tephras, altered first into bentonites and later, through burial metamorphism, into K-bentonites (metabentonites). These tephras were deposited as single crystals and glassy dust or pumiceous fragments in a restricted subtidal environment. The region of Famatina has previously been inferred as the source of abundant distal K-bentonites recorded in the adjacent lower-plate allochthonous Precordillera terrane. However, these K-bentonites within the proximal arc site were unknown and rather unexpected since they are generally better preserved like distal deposits, associated either with central vent plinian–ultraplinian eruptions or with accompanying co-ignimbrite ash clouds. Their chemistry and comparison with those K-bentonites in the Precordillera allow tracing an evolution from volcanic arcs into continental crust. K-bentonites described in this paper are much older than those recorded in the adjacent Precordillera terrane and seem to be associated with a first eruptive period along western Gondwana that has no counterpart in the Argentine Precordillera, suggesting a significant longitudinal separation between these two regions by the Early Ordovician.  相似文献   

The northern coast of the Ottnangian (middle Burdigalian,early Miocene) Molasse Sea in Germany: sediments,foraminiferal assemblages and biostratigraphy     

Martina Pippèrr  Bettina Reichenbacher  Gerhard Doppler  Mischa Hagmaier  Dietmar Jung 《International Journal of Earth Sciences》2016,105(3):1055-1085

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The effect of migratory shorebirds on the benthic species of three southwestern Atlantic Argentinean estuaries     

Florencia Botto  Oscar O. Iribarne  Mariano M. Martínez  Kaspar Delhey  Martina Carrete 《Estuaries and Coasts》1998,21(4):700-709

We experimentally evaluate the effect of migratory shorebirds on the benthic fauna of three southwestern Atlantic Argentinean stop-over and wintering sites: Bahía Samborombon (35°30′–36°22′S, 57°23′W), Mar Chiquita coastal lagoon (37°40′S, 57°26′W), and Bahía Blanca (38°48′–39°25′S, 50°–62°25′W). The experiments consisted of exclusion ceilings and controls (both 1 m²), with 10 replicates each and aligned at the same tidal level. During December 1994–May 1995 these experiments were done, twice in Bahía Samborombon, twice at two sites (Sotelo and Celpa) 4 km apart in Mar Chiquita coastal lagoon, and three times in Bahía Blanca. Three polychaete species (Laeonereis acuta, Nephtys fluviatilis, andHeteromastus similis) were found in similar densities in both areas of the Mar Chiquita lagoon.L. acuta andN. fluviatilis were affected in Sotelo, but there was no treatment effect in Celpa. In Sotelo the most abundant shorebirds were Hudsonian godwit (Limosa haemastica), American golden plover (Pluvialis dominica), and White-rumped sandpiper (Calidris fuscicollis), and in Celpa the most abundant shorebirds were White-rumped sandpiper, two-banded plower (Charadrius falklandicus), and lesser yellowlegs (Tringa flavipes). The largest polychaete densities were in the upper sediment layer (0–6 cm), which was also the most affected layer. Three polychaete species were found in Bahía Samborombon (L. acuta, H. similis, andNeanthes succinea), but onlyH. similis showed a treatment effect. The most abundant shorebirds in Samborombon were white-rumped sandpiper and two-banded plover. No effect was detected in Bahía Blanca, where the most abundant shorebirds were white-rumped sandpiper and American golden plover. In all cases, the species affected by shorebirds were the most abundant species. From the two sites of Mar Chiquita, there was a treatment effect only in Sotelo, which was also the area with higher shorebirds counts. However, much lower densities observed in Samborombon (similar to the unaffected area of Mar Chiquita) also produced a significant decrease in infaunal abundance. These evidences also suggest that just selection of study sites may produce different views of the interaction between shorebirds and benthic species.  相似文献