Biomes/Aquatic Biology

Cards (49)

  • Earths climate has the most significant influences on distribution of organisms
  • Four major components of climate: temperature, precipitation, sunlight and wind
  • Macroclimate: the climate of a large geographic area, such as a continent or region, over a long period
  • The two main components of macroclimate are solar energy and earths movement in space
  • Solar energy: the way light strikes the earth causes different temps depending on latitudes
  • Earths movement has to do with the titled axis that gives us different day lengths, solar radiation and temp
  • Other factosrs that influence macroclimate can be ocean currents and mountains
  • Mircoclimate: climate of localized small area, such as a valley or a pond.
  • Global Climate change: large scale changes in the earths climate causes by either human activity or natural disasters
  • Potential outcomes of global climate change: alteration of ocean currents, shrinking range of plants, habitat losses, and shifting biomes
  • Biome: major life zone characterized by a distinct climate, physical envrinment and vegetation.
  • Climate determines location of terrestrial biomes
  • Ecotone: transition of one type of habitat/ecosystem to another
  • Terrestrial biomes names are determined by the dominant plant type and the climate of the region.
  • Terrestrial biomes have vertical layering of vergitation
  • Aquatic Biomes are characterized by physical environment
  • There are two major categories: freshwater and marine
  • Freshwater: closely linked to soil and biotic components of surrounding environment and is influenced by patterns/speed of water flow
  • Marine: largest marine biomes, covers 75% of earths surface
  • Zonation: Physical and chemical layers
  • Two types of zonation: vertical and horizontal
  • Vertical Zonation: light absorption decreases with depth
  • Five zones in vertical zonation: photic zone, hphotic zone, abyssal zone, pelagic zone, and benthic zone
  • Photic zone: enough light for photosynthesis, highest primary production
  • Hphotic: no light and only consumers
  • Abyssal zone: deepest part of ocean (marine) and no light
  • pelagic zone: all water
  • Benthic Zone: The bottom of the ocean, where the sediment is the most dense.
  • Benthos: communities of detrivovers
  • Thermoclines: layers of water with significantly different temperatures
  • Spring turnover: surface area heats and ice melts, water becomes warmer, oxygen is at the bottom, and nutrients to the top
  • Fall turnover: air temps drops, water becomes cooler, oxygen moves to bottom and spreads nutrient through lake
  • Horizontal Zonation are different across marine and lakes
  • Horizontal Zonation in marine three zones: intertidal zone, neurotic zone, and oceanic zone
  • Intertidal zone: periodically exposed and submerged by tides
  • Neritic zone: from low tide to edge of continental shelf
  • Oceanic zone: open water
  • Horizontal zonation in lakes: littoral zone and limnetic zone
  • Littoral zone: shallow, well lit waters close to shore, plants are primary producers
  • Limnetic zone: father from shore and too deep for rooted plants