Historical Biogeography Flashcards
T/F
The Quaternary has been a time of biogeographic upheaval
true
because earth has passed through repeated cycles of glaciation
What era, period, and epoch are we currently in?
era: Cenozoic
period: quaternary
epoch: Holocene
- present interglacial epoch, started 12,000 years ago
Our current quaternary period is broken down into 2 epochs. What are they? When did each begin?
Pleistocene
- began 2.5mya
- glacial
Holocene (current)
- began 12,000yrs ago
- interglacial
What are the 3 models of Change over Earth’s History
- Predictable rules govern climate change: directional change, stable climate
- Random, abrupt, catastrophic events cause climate change (eg. asteroid impacts)
- The climate alternates between alternate stable states (eg. glacial/interglacial periods)
List up to 8 drivers of change on earth
- changing solar output
- tectonic and volcanic activity
- asteroid impacts
- methane clathrate releases
- orbital patterns (Milankovitch)
- changing ocean circulation
- changing sea levels
- humans
During the Pleistocene epoch, what were the 6 main climate forcing factors?
- Variation in the geometry of Earth’s orbit (Milankovitch)
- Variation in solar insolation emitted by the sun
- Plate tectonic processes: altered atmospheric and oceanic circulation and positions of continents
- Atmospheric absorptivity/reflectivity: Impact of volcanos
- Earth surface albedo (eg snow vs water vs soil vs vegetation)
- Feedback effects and interactions
Which epoch does this describe:
Period of gradual cooling during the mid-Cenzoic, followed by period
of dramatic climatic reversals
Pleistocene
During the pleistocene cooling, what was the consequence for plants and animals?
Regional assemblages of plants and animals that had co-evolved
during the warmth of Paleogene and Neogene were subject to
disruption and displacement
Ice extent during the last glacial maximum occurred approx. _____-_____ years ago
26,500-19,000 years ago
During the LGM, there were expansive ice sheets across much of both hemispheres. Which ice sheets remain today?
only greenland and antarctica
During the LGM, the average air temperatures over land were __-__C _____(warmer/cooler) than during interglacial periods
4-8C cooler
During the LGM, the ocean surface temperatures were __-__C ____ (warmer/colder) thank during interglacial periods
2-3C colder
During the LGM, was it on average drier or wetter compared to interglacial?
drier during LGM
generally, climatic zones shifted toward ___ ______ during glacial periods
the equator
during interglacial periods, climatic zones generally shift ____
poleward
the presence of ice during glacial periods also creates micro_____. Give 2 examples of these
microclimates
- air masses descending ice sheets would undergo adiabatic warming; makes glacial winters less severe & glacial summers colder/ less prone to heat waves
- some areas were wetter: eg. south of North America’s glaciers –> prevailing westerlies brought moisture from oceans = more water in American southwest lakes
How does moisture level generally shift during glacial periods?
Reduced solar heating= reduced evaporative input of water into the atmosphere
regional to global aridification and expansion of deserts and other xeric ecosystems
ie DRIER
Pluvial Lakes=
Formation of large lakes due to low
evaporation and high precipitation rates (in certain areas), fueled by prevailing winds carrying moisture from the ocean
give 3 examples of pluvial lakes
- remnants of one formed the great salt lake in utah
- death valley was a pluvial lake basin! now desert
- mojave desert (california)
In the deep past, were sea levels much higher or lower?
higher
Glacial/ interglacial periods can be interpreted from the ___ ____ at the time
sea level
lower sea level= glacial period because the water is locked up in ice sheets
higher sea level= interglacial
What are the 2 types of sea level changes? Define each
- Isostatic sea level changes –rising or lowering of the land surface relative to sea level
through movement of Earth’s crust - Eustatic sea level changes – alteration of the level of sea itself