Climate Flashcards
(30 cards)
Long term; global changes in the atmosphere
Climate
Where do these climate records come from
Proxies Ice cores Oxygen isotopes Foraminifera Tree rings Coral growth rings Leaf margins Habitat reconstruction
Anything that represents something else
Proxies
— tells us about the past temperatures
Paleotemperature proxy
Preserve tiny bubbles that hold atmosphere samples of carbon dioxide from when they crystallized
Ice cores
— is layered, so drilling into it all the way to the bottom you can count the —
Ice; rings/bands
— and — can tell us about temperature
Oxygen and water
Lots of ice sheets =
Ocean has a higher Oxygen 18/Oxygen16 ratio
No ice sheets =
Ocean has a lower Oxygen 18/Oxygen16 ratio
Ice sheets have a — Oxygen 18/Oxygen 16 ratio which makes the ratio in the ocean —
Lower; higher
— from H2O is recorded in — that oceans organisms produce
O2; calcite
Tiny organisms that make calcium carbonate skeletons
Foraminifera
Foraminifera become — to help produce climate records
Sediment in deep ocean
When climate gets warmer, 18O/16O ratio of seawater will —
Decrease
Foraminiferal O2 isotope and calculated temperature record is used for — temp records
Cenozoic
Oxygen isotopes are — and do not —
Stable; decay
Annual paleoclimate records
Tree rings
Tree rings grow in — conditions producing a new ring —
Favorable; every year
Tree rings are a — climate proxy
Localized
The — housed the oldest organism that was — years old
Bristlecone pine; 5000
Oxygen isotopes in carbon; records can be 1000s of years old
Coral growth rings
The — of the record is related to the — of the record
Length; resolution
How detailed the proxy record is
Resolution
How far back in time the proxy record can be used
Length