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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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Iberian abyssal plain (1)
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elements, isotopes
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carbon
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fossils
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coprolites (1)
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minerals
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Primary terms
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Atlantic Ocean
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North Atlantic
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Iberian abyssal plain (1)
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Northwest Atlantic (4)
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biogeography (1)
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Canada
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Eastern Canada
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Nova Scotia (1)
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Ontario (2)
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carbon
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Chordata
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Vertebrata
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Tetrapoda
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Theria
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continental shelf (1)
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Europe
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Iberian Peninsula (1)
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geophysical methods (2)
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Integrated Ocean Drilling Program
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Expedition 313
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IODP Site M0027 (3)
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IODP Site M0028 (2)
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IODP Site M0029 (3)
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Invertebrata
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Arthropoda
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Mandibulata
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Insecta
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Pterygota
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Neoptera
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Endopterygota
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Coleoptera (1)
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Diptera (1)
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Protista
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Thecamoeba (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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Sr-87/Sr-86 (1)
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land use (2)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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Ocean Drilling Program
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Leg 149
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ODP Site 898 (1)
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Leg 174A
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ODP Site 1072 (2)
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oxygen
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O-18/O-16 (1)
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paleoecology (3)
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paleogeography (1)
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palynomorphs
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Dinoflagellata (2)
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miospores
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pollen (2)
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Plantae
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algae
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Chlorophyta
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Charophyta (1)
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Desmidiales (1)
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diatoms (1)
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nannofossils (1)
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pollution (1)
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sea-level changes (1)
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sedimentary structures (1)
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sediments
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marine sediments (1)
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United States
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sedimentary structures
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coprolites (1)
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sedimentary structures (1)
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sediments
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sediments
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marine sediments (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Dung analysis of the East Milford mastodons: dietary and environmental reconstructions from central Nova Scotia at ∼75 ka years BP
The effect of acetolysis on desmids
Non-pollen palynomorphs as indicators of water quality in Lake Simcoe, Ontario, Canada
Chronology of Eocene–Miocene sequences on the New Jersey shallow shelf: Implications for regional, interregional, and global correlations
Sea-level control of New Jersey margin architecture: Palynological evidence from Integrated Ocean Drilling Program Expedition 313
Carbon-isotope stratigraphy from terrestrial organic matter through the Monterey event, Miocene, New Jersey margin (IODP Expedition 313)
SPECIAL ISSUE HONORING THE MEMORY OF PROFESSOR JOHN H. WRENN – AN INTRODUCTION
Abstract Palynomorphs are acid-resistant organic particles which behave aerodynamically and hydrodynamically like silt, and which resist degradation except in oxidizing or highly alkaline conditions. They are present in virtually all marine sediments, from the tropics to the poles and from estuarine to abyssal environments. Reconstructions of Quaternary sea level in cores from the New Jersey shelf (ODP Hole 1072A) and slope (ODP Hole 1073A) based on the modern distribution of palynomorphs across the New Jersey margin as well as the taphonomic alteration of palynological samples agree fairly well with data from other available proxies (e.g., oxygen isotopes). The palynological signatures of sediments on continental margins also provide information about the generation of sequences and sequence boundaries. The palynological character of surfaces identified as sequence boundaries from seismic reflection profiles records the generation of erosional unconformities during extreme lowstand events that altered the geometry of the margin. Very low palynomorph concentrations and presumably oxidized palynological assemblages (containing few protoperidinioid dinocysts or thin-walled pollen grains) characterize erosional unconformities. The strong seismic reflection associated with sequence boundaries results from physical contrast between the transgressive/highstand sediments (with very high palynomorph concentrations, P:D values declining rapidly upcore, and Pinus -dominated pollen assemblages) and underlying the lowstand sediments (with low palynomorph concentrations, high P:D values, taphonomically altered and ecologically mixed palynological assemblages). The palynological content of Quaternary sediments at ODP Sites 1072 and 1073 thus supports the role of eustasy as an important factor in shaping the New Jersey margin.