Скачать презентацию Ostracoda Ostracoda class of the Crustacea Size Скачать презентацию Ostracoda Ostracoda class of the Crustacea Size

Ostracoda.pptx

  • Количество слайдов: 9

Ostracoda Ostracoda

Ostracoda class of the Crustacea Size 0. 2 – 30 mm Fossil remains up Ostracoda class of the Crustacea Size 0. 2 – 30 mm Fossil remains up to 9 -10 cm 1 mm

Ostracoda Fresh and brackish water (lake, river, groundwater etc) Habitat Terrestrial (humid forest soils) Ostracoda Fresh and brackish water (lake, river, groundwater etc) Habitat Terrestrial (humid forest soils) Seawater (ocean floor and surface layer )

Factors of abundance Habitat characteristics: • Size, energy level, permanence of waterbody, depth of Factors of abundance Habitat characteristics: • Size, energy level, permanence of waterbody, depth of the site • Presence and types of aquatic plants • Availability of food • Predation Water characteristics: • • Temperature Salinity ad ionic composition p. H Dissolved oxygen content

Changing lake depth Shallow lake => plankton species Deep lake => benthos species Changing lake depth Shallow lake => plankton species Deep lake => benthos species

Water energy regime • Ostracods have about 8 -9 moult stages during their life Water energy regime • Ostracods have about 8 -9 moult stages during their life 1. Young and adult valves together => no strong current 2. Young absent => flows exist 3. Adult absent => unfavourable conditions for maturing

Salinity and ionic composition • Salinity and ionic composition of host waterbody are indicated Salinity and ionic composition • Salinity and ionic composition of host waterbody are indicated by degree of tolerance of ostracoda species to this variables • In temperate deep lakes benthic ostracode shell chemistry is related to isotopic water composition • In margunal marine settings ostracode shell chemistry is related to salinities

Geochemical analysis • Trace element content (Mg, Sr) => water temperature and water chemistry Geochemical analysis • Trace element content (Mg, Sr) => water temperature and water chemistry in both lakes and oceans • Stable isotope ratios (18 O/16 O, 13 C/12 C) – lake sediments, temperature and precipitation regime of the waterbody, CO 2 and dissolved inorganic carbon processes in the water • Indicator of past heavy metal pollution • Radiometric dating (radiocarbon and uranium series)

Thank you for attention! Thank you for attention!