(Table 1) Concentrations of amino acids in sediments from DSDP Site 68-502

In this chapter, we will report on the amino acids in the total acid hydrolysate of eight sediment samples from Leg 68 Site 502. This site was located on a topographic high at a depth of 3051 meters in the Colombian Basin of the western Caribbean Sea. Four holes were cored at the site by means of the hydraulic piston corer to a maximum sediment depth of 218 meters. The composite section is a virtually continuous, undisturbed sediment record covering almost 8 million years from the Holocene to late Miocene. Age estimates for the section are based on excellent magnetostratigraphic and biostratigraphic records. Four lithostratigraphic units (A, B, C, and D) were recognized, based on differences in color and content of clay, ash, foraminifers, and siliceous microfossils (Prell, Gardner, et al., 1980): A, yellowish brown to light brownish gray foraminifer-bearing (> 10%) nannofossil marl; B, gray to olive gray foraminifer-bearing nannofossil marl with occasional ash beds; C, light gray to dark greenish gray calcareous clay and foraminifer-bearing (< 10%) nannofossil marl; D, pale green to grayish green calcareous, ash-bearing clay with siliceous microfossils. The calcium carbonate content of these sediments increases from about 27 to about 49% from late Miocene to middle Pliocene (about 3.6 Ma) and remains uniform at about 48 to 50% from that time throughout the Quaternary. The eight sediment samples for amino acid analyses came from the third (502B) and fourth (502C) holes at Site 502. Samples ranged in sub-bottom depth from 4.3 to 225 meters spanning time from 0.3 to 7.7 Ma.

Revised chronology of Neogene DSDP holes from the World Ocean

After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this report we present newly revised age models for Neogene sediments from 94 DSDP holes. Biostratigraphic data for planktonic foraminifers, calcareous nannofossils, diatoms and radiolarians, paleomagnetic and other stratigraphic data were compiled from the original Initial Reports volumes of DSDP. The Berggren et al. (1985 doi:10.1130/0016-7606(1985)96<1407:CG>2.0.CO;2) scale was used for the age of magnetic reversals, and a variety of recent papers were used to establish a standard modern set of calibrations for marine microfossil events to the magnetic reversal scale. New age vs depth plots were made for each hole, and for each a new line of correlation was created. All tabulated stratigraphic data, new age models, and age depth plots are given as appendices to the report.

(Table 2) Stable isotopes in foraminifers at DSDP Leg 78

Analyses of stable isotopes of monospecific planktonic foraminifers (G. quadrilobatus group) and monogeneric benthic foraminifers (Cibicidoides spp.) from late Neogene Atlantic Site 502 and Pacific Site 503 were conducted in order to determine the paleoceanographic changes resulting from the late Neogene uplift of the Panama Isthmus and from climatic cooling. In general, results at each site are similar to those from previous studies for the late Miocene and late Pliocene time interval, documenting the late Miocene (6 Ma) shift in carbon isotopes and the inferred growth of permanent Northern Hemisphere continental ice sheets beginning about 3.2 Ma. Comparison of Atlantic-Pacific planktonic-benthic isotope data for four stratigraphic intervals (~6-8, ~5-6, ~3-5, and ~2-3 Ma) suggests that increasing isolation of Atlantic and Pacific low-latitude waters may be related to the emergence of the Panama Isthmus. The contrast between Atlantic and Pacific benthic foraminiferal d13C increased in two steps from 0.60 per mil to 1 per mil (the modern contrast) at about 6 Ma and 3 Ma. The first increase (0.15 per mil) may represent the end of previously limited deep-water communication between the Atlantic and Pacific at the present location of Panama. The second increase (0.25 per mil) may be due to increased production of North Atlantic Deep Water. This probably reflects the development of modern deep-sea circulation. The d18O of planktonic foraminifers begins to increase in Atlantic Site 502 at 4.2 Ma and may reflect the increasing salinity of the North Atlantic Ocean arising from diminishing surface-water exchange across Panama. This increase is clearly shown by contrasting the d18O of Atlantic and Pacific planktonic foraminifers, as well as the d18O of planktonic and benthic foraminifers at Site 502. This inferred increase in surface-water salinity begins at the time of increasing provinciality of Atlantic and Pacific planktonic foraminifers.

Stable isotope record of Cibicidoides wuellerstorfi from Pleistocene sediments of DSDP Site 86-502 in the Caribbean Sea

Variations in the stable isotopic composition of benthic foraminifera from Deep-Sea Drilling Project (DSDP) site 502B in the Caribbean Sea are used to reconstruct Atlantic intermediate water circulation variability over the last 1.2 m.y. Comparison of this record with other North Atlantic benthic isotope records indicates that Atlantic intermediate water circulation was relatively enhanced during glacial maxima when North Atlantic deep water (NADW) production was reduced. However, a simple, compensatory relationship between intermediate and deepwater circulation is not apparent. Geochemical models have shown that such changes in ocean circulation can affect atmospheric CO2 levels by changing vertical nutrient and alkalinity profiles. The Delta delta13C difference between Caribbean site 502B and deep equatorial Pacific site 677 is highly coherent and in phase with ice volume. Like the delta18O record, there is an increase in amplitude (40%) and a large increase in 100 kyr power after 0.7 Ma. The 1.2? Delta delta13C amplitude scales to 70 ppm V in atmospheric CO2 using Boyle's (1986) box model result. The implied increase in CO2 amplitude after 0.7 Ma may suggest a positive feedback role in effecting the higher-amplitude climatic fluctuations which characterize the last 0.7 m.y.

Stable carbon and oxygen isotope ratios of planktonic foraminifera from the equatorial Atlantic

Carbon isotopic records of nutrient-depleted surface water place constraints on the past fertility of the oceans and on past atmospheric pCO2 levels. The best records of nutrient-depleted delta13C are obtained from planktonic foraminifera living in the thick mixed layers of the western equatorial and tropical Atlantic Ocean. We have produced a composite, stacked Globigerinoides sacculifer delta13C record from the equatorial Atlantic, which exhibits significant spectral power at the 100,000- and 41,000-year Milankovitch periods, but no power at the 23,000-year period. Similar to the record presented by Shackleton and Pisias [1985], surface-deep ocean Delta delta13C produced with the G. sacculifer record leads the delta18O ice volume record. However, the glacial-interglacial amplitudes of Delta delta13C differ between our record and Shackleton and Pisias [1985] record. Although large changes in Delta delta13C occur in the equatorial Atlantic during early stages of the last three glacial cycles, surface-deep Delta delta13C at glacial maxima (18O stage 2, late stage 6, and late stage 8) was only about 0.2? greater than during the subsequent interglacial. Our results imply that nutrient-driven pCO2 changes account for about one third of the pCO2 decrease observed in ice cores, and consequently, Delta delta13C should not be used as a proxy pCO2 index. Enough variance in the ice core pCO2 records remains to be explained that conclusions about pCO2 and ice volume phase relationships should also be reexamined. As much as 40 ppm pCO2 change still has not been accounted for by models of past physics and chemistry of the ocean.

District Court of Queensland Act 1968 s 68 : jurisdiction in pre-proceedings applications under Personal Injuries Proceedings Act 2002

In Woolworths Ltd v Graham [2007] QDC 301 Searles DCJ struck out a pre-proceedings application under the Personal Injuries Proceedings Act 2002 (Qld)on the basis that the material before the Court was not sufficient to attract the jurisdiction of the District Court.The decision serves more broadly as a reminder that the District Court is an inferior court of defined and limited jurisdiction and that any proceedings brought in it must be demonstrably within the jurisdiction conferred on that court by legislation.

Rice ragged stunt oryzavirus genome segments S7 and S10 encode non-structural proteins of M(r) 68 025 (Pns7) and M(r) 32364 (Pns10) : brief report

The nucleotide sequences of genome segments S7 and S10 of a Thai-isolate of rice ragged stunt virus (RRSV) were determined. The 1938 bp S7 sequence contains a single large open reading frame (ORF) spanning nucleotides 20 to 1 843 that is predicted to encode a protein of M(r) 68 025. The 1 162 bp S10 sequence has a major ORF spanning nucleotides 142 to 1 032 that is predicted to encode a protein of M(r) 32364. This S10 ORF is preceded by a small ORF (nt 20-55) which is probably a minicistron. Coupled in vitro transcription-translation from the two major ORFs gave protein products of the expected sizes. However, no protein was visualised from S10 when the small ORF sequence was included. Proteins were expressed in Escherichia coli from the full length ORF of S7 (P7) and from a segment of the S10 ORF (P10) fused to the ORF of glutathione S-transferase (GST). Neither fusion protein was recognised by polyclonal antibodies raised against RRSV particles. Furthermore, polyclonal antibodies raised against GST-P7 fusion protein did not recognise any virion structural polypeptides. These data strongly suggest that the proteins P7 and P10 do not form part of RRSV particle. This is further supported by observed sequence homology (though very weak) of predicted.

Improving diagnosis of tumor-induced osteomalacia with gallium-68 DOTATATE PET/CT

Context: Tumor-induced osteomalacia (TIO) is a rarely diagnosed disorder presenting with bone pain, fractures, muscle weakness, and moderate-to-severe hypophosphatemia resulting from fibroblast growth factor 23-mediated renal phosphate wasting. Tumors secreting fibroblast growth factor 23 are often small and difficult to find with conventional imaging. Objective: We studied the utility of 68Ga-DOTA-octreotate (DOTATATE) somatostatin receptor positron emission tomography (PET)/computed tomography (CT) imaging in the diagnosis of TIO. Design and Setting: A multicenter case series was conducted at tertiary referral hospitals. Patients and Methods: Six patients with TIO diagnosed between 2003 and 2012 in Australia were referred for DOTATATE PET imaging. We reviewed the clinical history, biochemistry, imaging characteristics, histopathology, and clinical outcome of each patient. Results: Each case demonstrated delayed diagnosis despite severe symptoms. DOTATATE PET/CT imaging demonstrated high uptake and localized the tumor with confidence in each case. After surgical excision, there was resolution of clinical symptoms and serum phosphate, except in one patient who demonstrated residual disease on PET/CT. All tumors demonstrated high somatostatin receptor subtype 2 cell surface receptor expression using immunohistochemistry. Conclusions: In patients with TIO, DOTATATE PET/CT can successfully localize phosphaturic mesenchymal tumors and may be a practical first step in functional imaging for this disorder. Serum phosphate should be measured routinely in patients with unexplained muscle weakness, bone pain, or stress fractures to allow earlier diagnosis of TIO. - See more at: http://press.endocrine.org/doi/abs/10.1210/jc.2012-3642#sthash.eXD0CopL.dpuf

Comportamiento agroindustrial de veinticinco variedades de caña de azúcar (Saccharum sp. hibrido) en comparación con la variedad L 68-90 en caña planta

En el ciclo 90-91 se llevó a cabo el presente trabajo en el Ingenio Javier Guerra Báez con el objetivo de determinar el comportamiento agroindustrial de 25 cultivares de caña de azúcar en comparación con la variedad L 68-90. El experimento se sembró el 21 de febrero de 1990 en un suelo franco de la serie Nandaime, la cosecha se realizó a los 12 meses de edad el 21 de febrero de 1991. El diseño utilizado fue látice triple (5 x 5) y las variables estudiadas fueron: Germinación. Población, altura de tallos, diámetro de tallos, peso promedio de los tallos, rendimiento agrícola. rendimiento industrial y rendimiento agroindustrial Los datos fueron sometidos a un análisis de varianza y prueba de rangos múltiples de Duncan al 5% de significancia. Los mejores comportamientos para cada variable en estudio los obtuvieron los siguientes cultivares: Germinación: RB 73-2727, Cp 70-321, RB 77-3720, RB 73-2223, RB 73-9735 y RB 76-5288; Población: Sp 70-1423, Cp 70-321 RB 73-1012. Cp 71-6180. RB 73-1714. RB 76-5288. RB 73-2727, Cp 72-1210 y C 87-51; Longitud de tallo: RB 73-429. Cp 70-1527. RB 73-9735. RB 73-1012. Q 96 MEX 69-420 y MEX 68-P23; DiáMetro de los tallos: RB 73-2223, Cp 74-383. MEX 53-473, RB 76-5288. RB 73-9735. RB 73-5220. RB 73-9953. Cp70-1527, MEX 56-476 y MEX 68-p23; Peso promedio de los tallos: MEX 68- p23. RB 73-9735. RB 73-2223. CP 70-1527, RB 73-429. MEX 53-473. Q 96. MEX 69-420 y MEX 56-476;Rendimiento agrícola: Cp 71 -6180. MEX 68- P23. X 69-420. RB 73-1012. Sp 70-1423. RB 76-5288 y RB 73-9735; Rendimiento industrial Q 96, Cp 70-321, Cp 72-1210, MEX 68 P23 y Cp71-6180; Rendimiento agroindustrial Cp 71-6180.MEX 68-P23. Cp 70-321. RB 76-5288, Cp 72-1210. MEX69-420, RB 73-1012 Y Q96. Las variedades que presentaron enfermedades fueron: C 87-51, Cp 71-6180, Cp 70-1527, RB 73-2223. RB 73-2727. L '8-90, Cp 74-383, Sp 70-1284, RB 73-1714 y RB 73-429.

Evaluación agro-industrial de veinticinco variedades de caña de azúcar (Saccharum sp. hibrido), en comparación con la variedad L 68-90, en planta y retoño 1

El presente estudio corresponde a la evaluación de dos años de producción (90-91;91-92), de 25 variedades de caña de azúcar en comparación con la variedad L 68-90, establecido en el ingenio " Julio Buitrago Urroz ", para determinar su comportamiento agro­ industrial y seleccionar las mejores variedades para una segunda fase de selección. El ensayo se sembró 24 de marzo de 1990, la cosecha de planta se realizó el 21 de marzo de 1991, y el retoño 1 se cosecho el 21 de febrero de 1992. El diseño utilizado fue el de látice triple (5 x 5) parcialmente equilibrado y los parámetros estudiados fueron: Germinación, Población, Altura, Diámetro de los tallos, Peso promedio de los tallos, Rendimiento agrícola, Rendimiento industrial, y Rendimiento agro-industrial. Cada una de las variables fueron evaluadas mediante un análisis de varianza y a la prueba de rango múltiple de Duncan a un 5% de significación. Los resultados obtenidos fueron los siguientes: Germinación; Se obtuvieron diferencias altamente significativas, las mejores variedades son: Cp 70-321, Cp 70-1527, RB 73-9735, Mex 68-P23, RB 73-1012, Mex 53-473. Población; Se presentaron diferencias altamente significativas, resultando los mejores genotipos: Rb 73-2727, Cp 70-321, Sp 70-1423. Altura; Se determinó una alta diferencia significativa entre los cultivares destacándose: Sp 72-4790, RB 76-5288, RB 73-429. Diámetro de tallo; Se obtuvo una alta diferencia significativa siendo las mejores: RB 73-2223, Mex 56-476, Mex 69-420, RB 73-9735, Mex 53- 473, RB 73-9953, Cp 74-383. Peso promedio de los tallos; Se observó una alta diferencia significativa resultando los mejores genotipos: Mex 56-476, RB 73-2223, Mex 69-420, RB 73-429, Q 96, Mex 68-P23, RB 76-5288, RB 73-9735. Rendimiento agrícola; Estadísticamente se determinó una alta diferencia significativa, las variedades que superan al testigo son: Sp 72-4790, Sp 70- 1284, RB 73-9735. Rendimiento industrial; Se obtuvo diferencia significativa, siendo el mejor genotipo: La Q-96. Rendimiento agro-industrial; No se observaron diferencias significativas entre los cultivares en estudio, de acuerdo a la separación de medias las variedades más destacadas fueron: Sp 72-4790, RB 73- 5220. Respecto a las observaciones fitosanitarias la única variedad que no presento síntomas de las enfermedades señaladas en este estudio es: Sp 72-4790, las variedades más afectadas por el carbón son: RB 74-5672, Cp 72-1210, Cp 70-1527, RB 76-5288, RB 77-320, RB 73-1012, RB 73-9735, L 68-90.