695 resultados para Flyvbjerg, Bent


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Mode of access: Internet.

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Mode of access: Internet.

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Appendix A: List and discussion of scientific observations taken and calculated by M. Emile Roux, p. [359]-417. -- Appendix B: I. Natural history, p. 418-431; II. Vocabularies [and Mosso mass.] p.432-457; III. Material for the expedition, p. 458-460.

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A set of individual identification cards for rare and sensitive plant species found in the southeastern United States including Puerto Rico. Categories include forbs, shrubs, ferns, and trees. Each card has a color picture on one side and a description and map on the reverse. The description includes: family, flowering date, habitat, and identifying characteristics.

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Mode of access: Internet.

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Reprinted in part from various periodicals.

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Vols. for 1871-<76, 1913-14> include an extra number, The Christmas bookseller, separately paged and not included in the consecutive numbering of the regular series.

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Bibliography: v.1, p. 381-398; v.2, p. 445-466.

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Bibliography: p. 126-128.

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Verso of t.p.: Printed in the U.S.A. by The Quinn & Boden Company, book manufacturers, Rahway, New Jersey.

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"Open-file report."

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Inscribed for Earle Walbridge by the author.

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The Miocene Climatic Optimum (MCO; ~16.9 to 14.7 Ma) provides an outstanding opportunity to investigate climate-carbon cycle dynamics during a geologically recent interval of global warmth. We present benthic stable oxygen (d18O) and carbon (d13C) isotope records (5-12 kyr time resolution) spanning the late early to middle Miocene interval (18 to 13 Ma) at Integrated Ocean Drilling Program (IODP) Site U1335 (eastern equatorial Pacific Ocean). The U1335 stable isotope series track the onset and development of the MCO as well as the transitional climatic phase culminating with global cooling and expansion of the East Antarctic ice-sheet at ~13.8 Ma. We integrate these new data with published stable isotope, geomagnetic polarity and X-ray fluorescence (XRF) scanner-derived carbonate records from IODP Sites U1335, U1336, U1337 and U1338 on a consistent, astronomically-tuned timescale. Benthic isotope and XRF scanner-derived CaCO3 records depict prominent 100 kyr variability with 400 kyr cyclicity additionally imprinted on d13C and CaCO3 records, pointing to a tight coupling between the marine carbon cycle and climate variations. Our inter-site comparison further indicates that the lysocline behaved in highly dynamic manner throughout the MCO, with >75% carbonate loss occurring at paleo-depths ranging from ~3.4 to ~4 km in the eastern equatorial Pacific Ocean. Carbonate dissolution maxima coincide with warm phases (d18O minima) and d13C decreases, implying that climate-carbon cycle feedbacks fundamentally differed from the late Pleistocene glacial-interglacial pattern, where dissolution maxima correspond to d13C maxima and d18O minima. Carbonate dissolution cycles during the MCO were, thus, more similar to Paleogene hyperthermal patterns.