Search results for "DSDP ODP IODP sample designation"

showing 2 items of 2 documents

Planktonic foraminifera in ODP Hole 160-963A

2006

New faunal and floral records from Ocean Drilling Project Hole 963A, resolved at ?80-year spacing, provide evidence of suborbital scale climate variability in the central Mediterranean Sea throughout Marine Isotope Stage (MIS) 5. Cold events in the central Mediterranean Sea, indicated by low abundances of warm species and high abundances of cold species, are also evident in a planktonic foraminifera paleoclimatic curve. They have been linked to NGRIP Greenland ice core “C” events and appear correlative with similar sub-millennial climate fluctuations identified in the North Atlantic region and in the Alboran Basin (Westernmost Mediterranean). Low-resolution benthic and planktonic Oxygen Iso…

Counting >125 µm fractionOrbulina spp.Leg160Counting 125 µm fractionTurborotalia quinquelobaDEPTH sediment/rockOrbulina sppOcean Drilling Program (ODP)Neogloboquadrina pachyderma sinistralCounting >125 µm fractionAGENeogloboquadrina dutertreiGlobigerina bulloidesDSDP/ODP/IODP sample designationGloborotalia inflataDSDP ODP IODP sample designationSample code/labelGloborotalia scitula sinistralStainforthia davisiGlobigerinoides ruberJoides ResolutionGloboturborotalita tenellaSample code labelDrilling/drill rigDrilling drill rigsediment rockGloborotalia truncatulinoidesHastigerina siphoniferaDEPTHEarth System ResearchOcean Drilling Program ODPGlobigerinita glutinataNeogloboquadrina pachyderma dextralGloborotalia scitula dextral
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Stable isotopic composition of three foraminifera species in ODP Hole 160-963D

2020

Carbon-rich layers exist at both sides of the Mediterranean Sea sedimentary record and are called sapropels and organic rich layers (ORLs), respectively in the eastern and western basins. They have different levels of organic carbon accumulation and seafloor oxygen deprivation. The most recent sapropel and ORL deposition have a different timing, 10.8-6.1 and 14.5-9.0 ka respectively. Here we investigate oxygen isotopic records of three foraminifera species that occupy different habitats within the Sicily Channel water column since ~ 12.0 ka, thus in the sill between the eastern and western Mediterranean basins. These data are ice volume-corrected, to get information on water masses density …

Leg160Uvigerina spp. δ13CORLNeogloboquadrina incompta δ13C9.2 ka event8 2 ka eventDEPTH sediment/rockNeogloboquadrina incomptaGlobigerinoides ruber δ13CAGE8.2 ka event9 2 ka eventDSDP/ODP/IODP sample designationδ18ODSDP ODP IODP sample designationSample code/labelGlobigerinoides ruber δ18OSapropel S1Globigerinoides ruberJoides ResolutionUvigerina spp. δ18OSample code labelDrilling/drill rigDrilling drill rigsediment rockLIWDEPTHUvigerina sppδ13CEarth System ResearchNeogloboquadrina incompta δ18O
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