(Table 1) Sediment temperature and thermal conductivity at DSDP Leg 86 Holes

Using a new temperature recording instrument recently developed at the Woods Hole Oceanographic Institution, downhole temperature measurements were made at five sites during Deep Sea Drilling Project Leg 86. The instrument, which can be installed in the shoe of the hydraulic piston corer, allows measurements of sediment temperature to be made simultaneously with the collection of sediment cores. A numerical procedure was applied to correct the temperature disturbance caused by the corer's friction with the sediment. Detailed temperature profiles constructed from the data were combined with the measurement of thermal conductivity to calculate heat flow. Heat flow values were generally low at all sites of Leg 86, consistent with the age of the lithosphere (>100 m.y.) in the Northwestern Pacific Basin.

Characterization of late Campanian and Maastrichtian planktonic foraminiferal depth habitats and vital activities based on stable isotopes

Depth habitats of 56 late Cretaceous planktonic foraminiferal species from cool and warm climate modes were determined based on stable isotope analyses of deep-sea samples from the equatorial Pacific DSDP Sites 577A and 463, and South Atlantic DSDP Site 525A. The following conclusions can be reached: Planoglobulina multicamerata (De Klasz) and Heterohelix rajagopalani (Govindan) occupied the deepest plankton habitats, followed by Abathomphalus mayaroensis (Bolli), Globotruncanella havanensis (Voorwijk), Gublerina cuvillieri Kikoine, and Laeviheterohelix glabrans (Cushman) also at subthermocline depth. Most keeled globotruncanids, and possibly Globigerinelliodes and Racemiguembelina species, lived at or within the thermocline layer. Heterohelix globulosa (Ehrenberg) and Rugoglobigerina, Pseudotextularia and Planoglobulina occupied the subsurface depth of the mixed layer, and Pseudoguembelina species inhabited the surface mixed layer. However, depth ranking of some species varied depending on warm or cool climate modes, and late Campanian or Maastrichtian age. For example, most keeled globotruncanids occupied similar shallow subsurface habitats as Rugoglobigerina during the warm late Campanian, but occupied the deeper thermocline layer during cool climatic intervals. Two distinct types of "vital effect" mechanisms reflecting photosymbiosis and respiration effects can be recognized by the exceptional delta13C signals of some species. (1) Photosymbiosis is implied by the repetitive pattern of relatively enriched delta13C values of Racemiguembelina (strongest), Planoglobulina, Rosita and Rugoglobigerina species, Pseudoguembelina excolata (weakest). (2) Enriched respiration 12C products are recognized in A. mayaroensis, Gublerina acuta De Klasz, and Heterohelix planata (Cushman). Isotopic trends between samples suggest that photosymbiotic activities varied between localities or during different climate modes, and may have ceased under certain environmental conditions. The appearance of most photosymbiotic species in the late Maastrichtian suggests oligotrophic conditions associated with increased water-mass stratification.

Paleocene and Eocene nannofossil datums from Shatsky Rise and Walvis Ridge

The precision of late Paleocene to middle Eocene nannofossil datums is investigated by means of quantitative methods and correlated to the magnetic polarity stratigraphy, using sequences from the Northwest Pacific, Southeast Atlantic and Italy. It is the rule rather than the exception to find tails of very reduced abundances prior to, or after, a range of consistent and higher abundances. The absolutely first or final occurrence of a species, therefore, seldom provides a synchronous datum when material from different geographic areas are compared. On the other band, synchroneity is often confirmed when the initial sharp rise or the final sharp decline in abundance is used as datum level. The use of datums not employed in the two principal existing nannofossil zonal schemes can substantially improve the biostratigraphic resolution. Two established zonal markers show abundance patterns making them unsuitable as datums: the first occurrences of Ellipsolithus macellus (base NP4, diachronous) and Tribrachiatus nunnii (base NP10 and Paleocene/Eocene boundary, too rare and too short range in open ocean sections). The first occurrence of either Fasciculithus spp. or Sphenolithus spp. is a better marker near the base of NP4. The first occurrence of Discoaster diastypus at 56.6 Ma represents a suitable replacement for recognition of the Paleocene/Eocene boundary.

Strontium isotope ratios of planktonic foraminifera from sediment samples acroos the K/T boundary

Seawater 87Sr/86Sr values increase abruptly by 28 * 10**-6 across the Cretaceous/Tertiary boundary (KTB). This small, but rapid shift is superimposed on the larger scale structure of the seawater Sr isotope curve. The time scale of radiogenic Sr addition appears to be too rapid to reconcile with sources associated with volcanism, and we show that the amount of Sr required to produce even this small increase is too large to be derived from: (1) a KT bolide of the size constrained by the Ir anomaly, (2) continental crust ejecta from the impact of such a bolide, (3) soot from global wildfires initiated by an impact, or (4) any combination of these sources. The probable source of the radiogenic Sr is enhanced continental weathering, but the high rate of increase appears to rule out processes such as sea level regression, glaciation or tectonism. A plausible mechanism for rapid addition of radiogenic Sr to the oceans is enhanced weathering associated with globally distributed acid rain (pH c. 1) which is a proposed by-product of a bolide impact (Prinn and Fegley, 1987, doi:10.1016/0012-821X(87)90046-X).

(Table 1) Oxygen and carbon isotopic values of benthic foraminifera from the Upper Maastrichtian interval of various DSDP and ODP sites

Stable isotopic data from benthic foraminifera indicate the occurrence of at least three deepwater masses in the late Maastrichtian ocean. Given mean oceanic d18Ow of -1.0 per mil, the temperature of the coolest intermediate-depth waters was 5°-7°C, that of the deepest waters was 10°C, and that of the warmest intermediate waters was 13°-15°C. The cool intermediate-depth water mass probably originated in the high-latitude Southern Ocean. The deepest waters originated at least partly in the northern Atlantic. The source region for the warmest intermediate-depth water mass is unknown. Although much of the late Maastrichtian deep water was probably preconditioned for winter sinking by low- or middle-latitude evaporation, no more than ~11% of late Maastrichtian deep water could have been directly actuated by low-latitude sea surface evaporation. At least in the southern Atlantic and Indian Oceans, heat transport by upwelling of deep water was not the primary cause of mild sea surface and coastal temperatures.

Core alignment and composite depth scale of DSDP Site 86-577

Deep Sea Drilling Project Site 577 on Shatsky Rise (North Pacific Ocean) recovered a series of cores at three holes that contain calcareous nannofossil ooze of latest Cretaceous (late Maastrichtian) through early Eocene age. Several important records have been generated using samples from these cores, but the stratigraphy has remained outdated and confusing. Here we revise the stratigraphy at Site 577. This includes refining several age datums, realigning cores in the depth domain, and placing all stratigraphic markers on a current time scale. The work provides a template for appropriately bringing latest Cretaceous and Paleogene data sets at old drill sites into current paleoceanographic literature for this time interval. While the Paleocene Eocene Thermal Maximum (PETM) lies within core gaps at Holes 577* and 577A, the sedimentary record at the site holds other important events and remains crucially relevant to understanding changes in oceanographic conditions from the latest Cretaceous through early Paleogene.

Arreglos de siembra en el cultivo de la soya (Glycine max L.), variedad CEA-CH-86. Efecto sobre el crecimiento y rendimiento del cultivo

El presente trabajo se realizó con la finalidad de determinar el efecto de diferentes arreglos de siembra (0.3 metro entre surco por 7 plantas por metro lineal; 0.6 metro entre surco por 15 plantas por metro lineal: 0.6 metro entre surco por 18 plantas por metro lineal; O.7 metro entre surco por 25 plantas por metro lineal; 0.8 metro entre surco por 30 plantas por metro lineal y 0.9 metro entre surco por 36 plantas por metro lineal) sobre el crecimiento y rendimiento del cultivo de la soya (Glycine max L) variedad CEA-CH-86, bajo las condiciones ecológicas de la finca La Concepción, Nagarote León. El ensayo se estableció en la siembra de postrera de 1999, utilizándose un diseño de bloques completos al azar con cuatro repeticiones. Se encontró que los componentes de crecimiento (altura, diámetro y hojas por planta) presentaron diferencias a los 50 y 70 días después de la siembra y para las variables evaluadas para el rendimiento y sus principales componentes solamente se encontraron diferencias no significativas para el número de semillas por vainas y peso de mil granos. Los resultados del análisis de varianza indican que el arreglo de siembra 0.6 metro entre surco por 18 plantas por metro lineal obtuvo el mayor rendimiento (2,925.72 kg/ha) y la más alta tasa de retomo marginal {867. 16 por ciento).

Mejoramiento de dos componentes de sistema de producción del cultivo de la soya (Glycine max L.) variedad CEA-CH-86, su efecto sobre el crecimiento y rendimiento del cultivo

El presente trabajo se planificó con la finalidad de mejorar dos componentes del sistema tradicional de producción del cultivo de la soya (Glycine max L.) variedad CEA-CH-86. Por lo tanto, se trabajó con: densidades de siembra y períodos sin y con control de plantas indeseables para encontrar el período crítico de competencia de malezas. Para determinar la densidad óptima de siembra, se estableció un ensayo unifactorial en la época de primera de 2000 en donde se probaron seis densidades de siembra (238 095,250000, 297 619, 357 143, 378 788 y 396 825 plantas/ha. La densidad que indujo al mayor rendimiento se le determinó el período crítico de competencia de malezas, para lo cual se estableció un experimento unifactorial en donde se incluyeron tratamientos sin control y con control de malezas hasta los 20, 40, 60, 80, 100 y 120 dds. De las seis densidades evaluadas, la que dio el mayor rendimiento fue la de 297,619 plantas/ha con una producción de 2,300 kg/ha. Así mismo, se llegó a la conclusión de que el período crítico de competencia de maleza para el cultivo de la soya en la variedad CEA-CH-86 se determinó a partir de los 20 hasta los 60 días después de la siembra.

Evaluación de dosis de fósforo y potasio en el cultivo de la soya (Glycine max (L) Merr), variedad CEA-CH-86, su efecto sobre el crecimiento y rendimiento y su análisis económico

El presente trabajo se realizó con la finalidad de determinar el efecto de diferentes dosis de fósforo y potasio (10 kg/ha de fósforo – 30 kg/ha de potasio; 20 kg/ha de fósforo – 40 kg/ha de potasio; 30 kg/ha de fósforo – 50 kg/ha de potasio; 40 kg/ha de fósforo – 60 kg/ha de potasio) y un tratamiento testigo (sin aplicación de fósforo y potasio) sobre el crecimiento y rendimiento del cultivo de la soya ( Glycine max (L) Merr.) variedad CEA- CH-86, bajo las condiciones ecológicas de la finca La Concepción, ubicada en el municipio de Nagarote departamento de León. El ensayo se estableció en la siembra de postrera del 2003, utilizándose un diseño de bloques completos al azar con cuatro repeticiones. Se encontró que los componentes del crecimiento (altura, diámetro y hojas por planta) presentaron diferencias significativ as a los 50 y 70 días después de la siembra, y para las variables correspondientes a los componentes del rendimiento y sus principales componentes solamente se encontraron diferencias no significativas para el número de granos por vainas. Los resultados del análisis de varianza indicaron que cuando se aplicó 30 kg/ha de fósforo – 50 kg/ha de potasio se obtuvo el mayor rendimiento (1 930 kg/ha), el mayor beneficio neto (1 361.37 C$ / ha) y la mas alta tasa de retorno marginal (197.10 por ciento).