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  • 130-806B; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Globigerinoides sacculifer sac, δ18O; Intercore correlation; Joides Resolution; Leg130; Mass spectrometer Finnigan MAT 251; North Pacific Ocean; Ocean Drilling Program; ODP  (1)
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  • 1
    Publication Date: 2021-06-27
    Description: The recovery of benthic communities inside the western Gulfof Maine fishing closure area was evaluated by comparing invertebrate assemblages at sites inside and outside of the closure four to six years after the closure was established. The major restriction imposed by the closurewas a year-round prohibition of bottom gillnets and otter trawls. A total of 163 seafloor sites (~half inside and half outside the closure) within a 515-km2 study area were sampled with some combination of Shipek grab, Wildco box corer, or underwater video. Bottom types ranged from mud (silt and clay) to boulders, and the effects of the closure on univariate measures (total density, biomass, taxonomicrichness) of benthos varied widely among sediment types. For sites with predominantly mud sediments, there were mixed effects on inside and outside infauna and no effect onepifauna. For sites with mainly sand sediments, there were higher density, biomass, and taxonomic richness for infauna inside the closure, but no significant effects on epifauna. For sites dominated by gravel (which included boulders in some areas), there were no effects on infauna but strong effects on epifaunal density and taxonomic richness. For fishing gear, the data indicated that infauna recovered insand from the impacts of otter trawls operated inside the closure but that they did not recover in mud, and that epifauna recovered on gravel bottoms from the impact of gillnets used inside the closure. The magnitudes of impact and recovery, however, cannot be inferred directly from ourdata because of a confounding factor of different fishing intensities outside the closure for a direct comparison ofpreclosure and postclosure data. The overall negative impact of trawls is likely underestimated by our data,whereas the negative impact of gillnets is likely overestimated.
    Keywords: Biology ; Ecology ; Fisheries
    Repository Name: AquaDocs
    Type: article , TRUE
    Format: application/pdf
    Format: application/pdf
    Format: 308
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  • 2
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    PANGAEA
    In:  Supplement to: Jansen, Eystein; Mayer, Larry A; Backman, Jan; Leckie, R Mark; Takayama, Toshiaki (1993): Evolution of Pliocene climate cyclicity at Hole 806B (5-2 Ma): oxygen isotope record. In: Berger, WH; Kroenke, LW; Mayer, LA; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 130, 349-362, https://doi.org/10.2973/odp.proc.sr.130.028.1993
    Publication Date: 2024-01-09
    Description: A detailed Pliocene oxygen isotope record from the Ontong Java Plateau, based on measurements of the surface-dwelling planktonic foraminifer Globigerinoides sacculifer, was produced for the period from 5 to 2 Ma. The record documents major long- and short-term climate changes. The results show periods of enhanced ice volume at 4.6 to 4.3 Ma and after 2.85 Ma, a long-term warming trend from 4.1 to 3.7 Ma, and a distinct cooling trend that was initiated at 3.5 Ma and progressed through the initiation of large-scale Northern Hemisphere glaciation after 2.85 Ma (according to the time scale of Shackleton and others proposed in 1990). Periods of high average ice volumes also show the highest d18O amplitudes. The pattern of climate cyclicity changed markedly at about 2.85 Ma. Earlier times were marked by high-frequency variability at the precessional frequencies or even higher frequencies, pointing to low-latitude processes as a main controlling factor driving planktonic d18O variability in this period. The high-frequency variability is not coherent with insolation and points to strong nonlinearity in the way the climate system responded to orbital forcing before the onset of large scale Northern Hemisphere glaciation. After 3 Ma, stronger 41-k.y. cyclicity appears in the record. The shift in pattern is clearest around 2.85 Ma (according to the time scale proposed by Shackleton and others in 1990), 100-200 k.y. before the most dramatic spread of Northern Hemisphere ice sheets. This indicates that high-latitude processes from this point on began to take over and influence most strongly the d18O record, which now reflects ice-volume fluctuations related to the climatic effects of obliquity forcing on the seasonality of high-latitude areas, most probably in the Northern Hemisphere. The general Pliocene trend is that high-latitude climate sensitivity and instability was increasing, and the causal factors producing the intensified glacial cyclicity during the Pliocene must be factors that enhance cooling and climate sensitivity in the subarctic areas.
    Keywords: 130-806B; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Globigerinoides sacculifer sac, δ18O; Intercore correlation; Joides Resolution; Leg130; Mass spectrometer Finnigan MAT 251; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 2084 data points
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