Two year time-series fluxes of Silicoflagellates and Actiniscussize fractioned results from subarctic Pacific Station Papa, 1982-1984
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Woods Hole Oceanographic Institution , Woods Hole, Mass
Silicoflagellates -- North Pacific Ocean., Actiniscus pentasterias -- North Pacific Ocean., Marine sediments -- North Pacific O
|Series||WHOI -- 85-41., Technical report, WHOI (Series) -- 85-41., Technical report (Woods Hole Oceanographic Institution)|
|Contributions||Woods Hole Oceanographic Institution.|
|LC Classifications||QK569.S53 T32 1985|
|The Physical Object|
|Pagination||iii, 53 p. :|
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Takahashi K () Seasonal fluxes of silicoflagellates and Actiniscus in the subarctic Pacific during – J Mar Res – CrossRef Google Scholar Takahashi K, Billings JD, Morgan JK () Oceanic province: assessment from the time-series diatom fluxes Cited by: 3.
Takahashi, K., Two Year Time-series Fluxes of Silicoflagellates and Actiniscus: Size Fractioned Results from subarctic Pacific Station PAPA, – Woods Hole Oceanographic Institution Technical Report, WHOI, by: The time series sediment trap samples were collected for 4 to day periods depending on the samples; most of the samples were collected for 14 to day periods.
From a depth of m, a total of 47 samples represents a nearly two-year continuous record of the fluxes of silicoflagellate and Actiniscus : Kozo Takahashi and 孝三 高橋. In order to evaluate their value as productivity or temperature indicators, species of silicoflagellates and Actiniscus, a dinoflagellate genus with siliceous endoskeletons, were examined from the time series trap samples.
Their fluxes were enumerated for a total of samples from Station Papa and 24 samples from Station by: To study the temporal variability of oceanic productivity, time series particle fluxes were monitored at pelagic Station Papa (50°N, °W) in the eastern subarctic Pacific from September thro Cited by: Two Year Time-series Fluxes of Silicoflagellates and Actinis-cus: Size Fractioned Results from subarctic Pacific Station PAPA, – Mineral flux and biogeochemical cycles of marine.
To study the temporal variability of oceanic productivity, time series particle fluxes were monitored at pelagic Station Papa (50°N, °W) in the eastern subarctic Pacific from September through August Automated Particle Flux (PARFLUX) time series sediment traps were deployed at m and m in the m deep pelagic ocean.
The traps collected samples for 2-week periods for. Seasonal and vertical flux variations of coccolithophorids, discrete coccoliths, silicoflagellates, ebridians, and diatoms were investigated using time-series sediment traps deployed in the central Black Sea for 2 years from September through August (Year 1) and from October through September (Year 2).
Silicoflagellates Fluxes in the traps and accumulation rates in the sediment are expressed as individuals m −2 year −1. a Data are taken from Lange et al. (Lange et al., ). Yearly fluxes – Traps a × 10 8 × 10 7 × 10 8 × 10 7 × 10 8.
Fluxes of silicoflagellates, the dinoflagellate Actiniscus sp., In contrast, time-series sediment trap samples integrate production year-round (mean, g C m-2 d-l), with peak values reaching g C m-2 d- l in June-July and lower values in winter (Schemainda et al.
Fluxes of silicoflagellates, the dinoflagellate Actiniscus sp., polycystine and phaeodarian radiolarians, tintinnids, ciliate(?) cysts, and pelagic molluscs were estimated for 13 sediment trap.
Time-series flux variabilities of biogenic opal particles were m deep Two year time-series fluxes of Silicoflagellates and Actiniscus book, yielding nearly continuous time-series flux records for four years.
The flux data allowed us to examine interannual and seasonal Seasonal fluxes of silicoflagellates and Actiniscus in the subarctic Pacific duringJ. Mar. Res., 45,la.
To study the temporal variability of oceanic productivity, time series particle fluxes were monitored at pelagic Station Papa (50°N, °W) in the eastern subarctic Pacific from September through August Automated Particle Flux (PARFLUX) time series sediment traps were deployed at m and m in the ‐m deep pelagic ocean.
The traps collected samples for 2‐week periods. Micropaleontology 55(), Onodera, J., and K.
Details Two year time-series fluxes of Silicoflagellates and Actiniscus FB2
Takahashi () Middole Eocene ebridians from the central Arctic aleontology 55(), Onodera, J., and K. Takahashi () Taxonomy and biostratigraphy of middle Eocene silicoflagellates in the central Arctic Basin. Micropaleontology 55(), Silicoflagellates and Actiniscus: vertical fluxes at Pacific and Atlantic sediment trap stations Takahashi, Kozo (Woods Hole Oceanographic Institution, ) Vertical fluxes of silicoflagellate skeletons were measured in meso- and bathypelagic zones at four PARFLUX sediment trap stations located in the Pacific and Atlantic oceans.
Takahito Ikenoue, Kozo Takahashi and Seiji Tanaka, Fifteen year time-series of radiolarian fluxes and environmental conditions in the Bering Sea and the central subarctic Pacific, –, Deep Sea Research Part II: Topical Studies in Oceanography, /,(), (). The time series sediment trap samples were collected for 4 to day periods depending on the samples; most of the samples were collected for 14 to day periods.
From a depth of m, a total of 47 samples represents a nearly two-year continuous record of the fluxes of silicoflagellate and Actiniscus taxa. The value of N s, averaged over the depth range (5– m) for each year at all stations deeper than m and located within the geographic area bounded by –°N and –°W, increased 25% between andwith the maximum being observed in The decrease in is due to data being collected one month later than.
Two year time-series fluxes of Silicoflagellates and Actiniscus: size fractioned results from subarctic Pacific Station Papa, / Kozo Takahashi. Woods Hole, Mass.: Woods Hole Oceanographic Institution, W2 no the column (Fig.
This paper does not specify which taxa have been reworked from the older sediments, but the characteristic fossils for the Sarmatian period are given in table 2.
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Tab. Stratigraphic position of Sarmatian based on phytoplankton in the Central Paratethys Phytoplankton zones 03 =t wo Calcareous nannoplankfon Silicoflagellates.
Takahashi, K., Plankton shell fluxes and biological productivity in the subarctic regions of the Pacific Ocean. Bull. Plankton Soc. Japan, 43(2),Takahashi, K.
Time-series fluxes of Radiolaria in the eastern subarctic Pacific Ocean. News of Osaka Micropaleonotologists, Special Volume No.
Onodera, J., E. Watanabe, S. Nishino, N. Harada () Distribution and vertical fluxes of silicoflagellates, eburidians and the endoskeletal dinoflagellate Actiniscus in the in the western Arctic Ocean.
Polar Biology (accepted) 22 Aug A general investigation was made of the thermal expansion of various silicate fluxes The fluxes considered in the crystalline (anisotropic) and glassy (isotropic) states. were ten feldspars, two nepheline syenites, anorthosite, aplite, and lepidolite.
Benthic vegetation at the land-water interface is recognized as a filter for silica fluxes, which represents an important but under-investigated subject. This paper aims to analyze stocks and fluxes of biogenic (BSi) and dissolved (DSi) silica in relation to nitrogen (N) and phosphorus (P) in the littoral zone of a deep lake.
Specifically, we evaluated how different primary producers can.
Description Two year time-series fluxes of Silicoflagellates and Actiniscus EPUB
Study Site. The sampling station (point B) is located at the entrance of the Bay of Villefranche-sur-Mer (43° N, 7° E; water depth ~85 m), on the northern coast of the Ligurian Sea, NW Mediterranean Sea (Fig.
1).It is characterized by low chlorophyll-a concentrations , and is part of the “intermittent blooming” eco-region of the Mediterranean Sea . Figure shows the two segmented components when the bottom-hole node is selected: reservoir and tubing components.
For a given production rate, the bottom-hole pressure can be calculated in two ways: 1) from the reservoir component using inflow equations and 2) from the tubing component using multiphase flow correlations for pipes and chokes.
In our time series, only the years with the most extreme NAO winter values (Fig. 3) reflected the hypothesis advanced by Gómez and Gorsky (Gómez and Gorsky, ): during the NAO index showed the most negative values of the record and high diatom valve fluxes were recorded, whereas during the NAO winter index exhibited its highest.
CiteScore: ℹ CiteScore: CiteScore measures the average citations received per peer-reviewed document published in this title.
CiteScore values are based on citation counts in a range of four years (e.g. ) to peer-reviewed documents (articles, reviews, conference papers, data papers and book chapters) published in the same four calendar years, divided by the number of.
Introduction. Resolving records of global change through the most recent deglaciation event (18–11 ka) is one of the primary challenges to developing cohesive and robust theories regarding rapid climate change .The last deglaciation was a profound event in the global climate system, wherein atmospheric [CO 2] increased by 80– ppmv [2, 3], global average temperature rose 3–4°C.
Two systems are to operate in parallel. Two transformers are to operate in parallel. Connecting two different lines originating from the same source. In a three phase system the voltage or current sinusoid attain peak values periodically one after another. The sinusoid are. Soil Mechanics: concepts and applications 2nd edition are on the website of the publisher and can be ordered from @ or phone: +44 (0) First published by Spon Press, an imprint of Taylor & Francis, 2 Park Square, Milton Park, Abingdon, Oxon OX14 4RN.
d, Time series of organic δ 15 N (organic) and δ 13 C (average of the planktonic foraminifera Gb and Nps) as a time series; these data form the comparison in c.In this study we will summarize and evaluate the particle flux measurements made with sediment traps developed at Oregon State University between and ().The OSU trap is a single-cone modification of a design originally developed by Andrew Soutar (Soutar et al., ).
It features all plastic or fiberglass construction, a two-to-one height to diameter cone, a one cm by five cm baffle.
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