Marine Sediments M a r i n e S e d OCEN 10: Foothill College m Dr. Christopher DiLeonardo Geology & Oceanography Departments i e General Oceanography n t s M S e a d i m r n e i The Process of Sedimentation e n t s • Particles of material that accumulate on the sea floor – Solid rock fragments, precipitated minerals, & organism “hard parts” (shells, skeletons, etc.) • Preserve evidence of the past M S e a d i m r n e i – Provide information about sediment transport, tectonics, climate, ecosystems, etc. – Rocks made from marine sediments may contain fossils (preserved portion of plant or animal), which provide direct evidence of past life e n t s 1 M S e a d i m r n e i Sediment Types & Sources e n t s 4 Major Types of Marine Sediments M a r i n e S • Lithogenous d • Biogenous m • Hydrogenous e i e • Cosmogenous n t s Lithogenous Sediments M S e a d i m r n e i e n t • Originate from continental land masses, volcanic activity in the open ocean, and/or glacial activity • Major constituents include: – – – – – Quartz (pure silicate… just Si & O) Feldspars (K and Na silicates) Mica (K, Al silicate) Clay minerals Rock fragments s 2 Basalt (Oceanic crust) Granite (Continental crust) Weathering of rocks rich in ferromagnesian minerals produce clays (and Fe & Mg ions); rocks rich in non-ferromagnesian minerals generate silicate mineral grains M S e a d i m r n e Lithogenous Sediment i e n t s 3 Lithogenous Sediments • Particle size is used to distinguish between the various types of lithogenous sediment M S e a d i m r n e Biogenous Sediment i e n t s 4 Biogenous Sediments • Organically produced particles… namely, calcium carbonate (CaCO3) or silica (SiO2) • Silica comes from diatoms (algae) & radiolarians (animals) • Calcium carbonate mostly from foraminifera (animals) & coccolithophores (algae) Coquina Coral reef material & stromatolites are other forms of calcareous deposits Stromatolite Mounds M S e a d i m r n e Hydrogenous Sediment i e n t s 5 Hydrogenous Sediments • Manganese Nodules • Phosphorites Hydrogenous Sediments Glauconite – greenish hydrous Fe, K silicate of complex & variable composition Carbonates – mostly biogenic, but non-biogenic types also occur Hydrogenous Sediments Evaporites – salt minerals that precipitate as sea water evaporates Metal Sulfides – hydrothermal vent deposits 6 M S e a d i m r n e Cosmogenous Sediment i e n t s M S e a d i m r n e Depositional Systems i e n t s 7 Depositional Systems M S a d i m r n e • Neritic Sediment Deposits – Found near the continents and show a variety of particles sizes – Mostly lithogenous sediment entering from shore and transported across marine provinces e i • Pelagic Sediment Deposits e – Fine grained sediments that collect slowly on deep ocean floor – Lithogenous, biogenous, and hydrogenous sediments common (but in different regions) n t s Neritic Depositional Systems • Beach Deposits M a r i n e S • Relict Sediments d • Turbidites e i • Glacial Deposits e • Stromatolites m n t s Pelagic Depositional Systems • Abyssal clay • Oozes – Calcareous – Siliceous 8 Biogenous Sediment Accumulation • Rate of accumulation depends on: sedimentation rate, degree of preservation, & amount of other materials (clays) deposited Pelagic Sediment Deposits 9
© Copyright 2026 Paperzz