The modulation potential used in the calculations is based on the composite of data determined from the cosmogenic
isotope records of 10Be and a neutron monitor.
«The surface temperature changes for the last 4000 years in northern inland Iberia (an area particularly sensitive to climate change) are determined by a high resolution study of carbon stable
isotope records of stalagmites from three caves (Kaite, Cueva del Cobre, and Cueva Mayor) separated several 10 s km away in N Spain.
Diatom and stable
isotope records of late Holocene lake ontogeny at Indrepollen, Lofoten, N.W. Norway: a response to glacio - isostacy and Neoglacial cooling., The Holocene, 19, 261 - 271.
For the Holocene, the cosmogenic
isotope records of 10Be from WAIS Divide and 14C for IntCal13 demonstrated that WD2014 was consistently accurate to better than 0.5 % of the age.
Their results overcome a basic problem of trying to discern the deep history of ice from bedrock: every time an ice sheet retreats and then grows back, it scours away the bedrock and
the isotope record of its own past.
«Oxygen and Carbon
Isotope Record of East Pacific Core V19 - 30: Implications for the Formation of Deep Water in the Late Pleistocene North Atlantic.»
We use the rich climate history of the Cenozoic era in the oxygen
isotope record of ocean sediments to explore the relation of climate change with sea level and atmospheric CO2, inferring climate sensitivity empirically.
Not exact matches
The ratio
of strontium to calcium in a given layer
of coral reef — as well as the amount
of a heavier
isotope of oxygen in the carbonate itself — reflect the temperature in this historical
record, but the isotopic information also reveals rainfall.
In Greenland lead
isotopes in ice cores reveal a
record of lead pollution from Roman smelting in Spain some 2,000 years ago.
«Any potential [spike] would have both the radionuclide
record as well as the SCP one — as well as a few invasive species, bits
of microplastic and stable carbon
isotopes,» explains geologist Jan Zalasiewicz
of the University
of Leicester in England and chairman
of the working group that is evaluating whether or not to add the Anthropocene to the geologic timescale.
«A lot
of this rests on the carbon
isotope analysis,» Rothman says, which is exceptionally strong and clear in this part
of the geological
record.
The team used
records of oxygen
isotope ratios (which provide a
record of ancient water temperature) from microscopic plankton fossils recovered from the Mediterranean Sea, spanning the last 5.3 million years.
That could explain two other anomalies from the era's geologic
record, Lenton says: the large amounts
of organic - rich shale that were deposited as nearshore sediments and the unusually high proportion
of carbon - 13
isotopes in the rocks.
They write, «The occurrence
of humid periods previously identified in lacustrine or speleothem
records highlights the complexity and heterogeneity
of the Arabian paleoclimate, and suggests that interior migration pathways through the Arabian Peninsula may have been viable approximately every 23,000 years since at least marine
isotope state (MIS) 6,» about 191 thousand years ago.
By carefully micro-sampling each shell along its direction
of growth and analyzing for stable carbon and oxygen
isotopes and trace elements, the team reconstructed a
record of seasonal variation during the lifetimes
of the organisms.
Brown researchers have compiled a detailed Indonesian climate
record of the last 60,000 years, tracking telltale indicators in sedimentary cores: titanium levels (a marker for surface water runoff) and the carbon
isotopes of leaf wax, a marker for plant varieties (grasses indicate dry conditions).
The researchers compared the lead
isotopes in their sediment samples with those found in preserved Roman piping to create a historical
record of lead pollution flowing from the Roman capital.
The extra mass
of the exotic antiquark is enough to make this antihydrogen
isotope heavier than the previous
record - holder, antihelium.
Fisher, who studies the extinction
of mastodons and mammoths, suggests some answers could lie in nitrogen
isotopes in the Patagonian bones, which can
record changes in an animal's diet and, thus, its environment.
For example, rock
records of an
isotope of strontium — 87Sr — seem to show an increase in so - called chemical weathering, or weathering that is not simply the result
of rain or other natural but not life - related processes.
By studying the variations
of uranium
isotopes recorded in carbonates, the team was able to infer global anoxia occurring throughout the ocean using samples from a single outcrop.
In the past decade, paleoclimatologists have reconstructed a
record of climate change over the last millennium by consulting historical documents and examining indicators
of temperature change like tree rings, as well as oxygen
isotopes in ice cores and coral skeletons.
Whenever they found large dips in the oxygen - 18
isotope, they found a corresponding historical
record of a hurricane.
Eggshells contain carbon, which comes from the birds» diets, and because different plants have different ratios
of carbon
isotopes, the shells can be used as a rough
record of what birds ate.
The difference between using DNA analysis and
isotope tracking is a variation on the nature versus nurture debate: DNA
records an organism's genetic inheritance, and
isotopes reflect the composition
of the environment in which it grows.
The oxygen and carbon
isotopes present in the remains provided them with
records of temperature and humidity levels during the period.
The paleoclimate data, which included mainly changes in the oxygen
isotopes of the calcium carbonate deposits, were then compared to similar
records from other caves, ice cores, and sediment
records as well as model predictions for water availability in the Middle East and west central Asia today and into the future.
In both cases the climate
records are based on oxygen
isotope measurements on datable layers
of ice or stalagmite cave deposition.
Because plants preferentially use the lighter
isotope, its scarcity is a
record of how much life the oceans supported.
«As an animal eats and drinks, the local strontium
isotope composition
of the water, plants and animals consumed is
recorded in its skeletal tissues.»
New evidence
of Holocene climate and atmospheric circulation variability, inferred from lacustrine stable
isotope records from Gotland, southern Sweden Francesco Muschitiello, Dan Hammarlund, Barbara Wohlfarth
Wang, Lean, and Sheeley (2005) compared a flux transport model with geomagnetic activity and cosmogenic
isotope records and to derive a reconstruction
of TSI since 1713.
Biomineralisation influences on boron
isotopes are then explored, addressing the apparently contradictory observations that foraminifera manipulate pH during chamber formation yet their δ11B appears to
record the pH
of ambient seawater.
Evidence from carbon
isotope records from both soil carbonates [18]--[20] and biomarkers (n - alkanes) extracted from deep - sea sediments [21] provide clear evidence
of a progressive vegetation shift from C3 (∼ trees and shrubs) to C4 (∼ tropical grasses) plants during the Plio - Pleistocene.
There are also a number
of paleoclimatic recorders
of oxygen
isotopes, including lake / ocean
records, speleothems (in caves), corals, ice cores, etc..
First, I do think that there is a lot
of work to be done in the interpretation
of oxygen / hydrogen
isotope values obtained at a site, and there's still plenty
of disagreement in the paleo - community on how to best connect the isotopic signal in a
record with climate.
This absence is reflected in numerous proxies, particularly the
record of mass - independent fractionation
of sulfur
isotopes.
According to the researchers, this
isotope formed as a result
of cosmic ray particles or protons hitting out atmosphere, emanating from a minor superflare, around 10 — 100 times larger than any solar flare in
recorded history.
Based on the temperature minimum
recorded from the early Late Oxfordian
of Kachchh, it was suggested that the widening
of the Trans - Gondwanan Seaway may have led to increased upwelling in the Malagasy Gulf and to a cooling
recorded in the oxygen
isotopes of belemnites and other marine invertebrates from Kachchh [38].
A fossil is the remains or traces
of a once - living plant or animal that was preserved in rock or other material before the beginning
of recorded history Carbon - 14, 14 C, or radiocarbon, is a radioactive
isotope of carbon with an atomic nucleus containing 6 protons and 8 neutrons.
Improved source apportionment
of PAHs and Pb by integrating Pb stable
isotopes and positive matrix factorization application (PAHs): A historical
record DATING DOULTON BURSLEM.
For this rare Philadelphia appearance, he performs with the collective Digital Primitives featuring Israeli tenor saxophonist and bass clarinetist Assif Tsahar, known for his work with Cecil Taylor, Rashied Ali, Peter Kowald, William Parker and Hamid Drake; and drummer Chad Taylor, a member
of the Chicago Underground Duo and Iron and Wine, and a major contributor to Chicago's post-rock scene where he has
recorded or collaborated with Tortoise,
Isotope 217, Stereolab, Sam Prekop and Jim O'Rourke.
As a starting point, we explore what the traces
of the Anthropocene will be in millions
of years — carbon
isotope changes, global warming, increased sedimentation, spikes in heavy metal concentrations, plastics and more — and then look at previous examples
of similar events in the geological
record.
The afternoon sessions on water
isotopes in precipitation was quite exciting because
of the number
of people looking at innovative proxy archives, including cave
records of 18O in calcite, or deuterium in leaf waxes, which are extending the coverage (in time and space)
of this variable.
We only have direct observations
of total solar irradiance (TSI) since the beginning
of the satellite era and substantial evidence for variations in the level
of solar activity (from cosmogenic
isotopes or sunspot
records) in the past.
To replicate the observed isotopic offset, the model requires that enhanced levels
of organic - carbon and pyrite burial continued a few hundred thousand years after peak organic - carbon burial, but that their
isotope records responded differently due to dramatically different residence times for dissolved inorganic carbon and sulfate in seawater.
We analyzed stable carbon and oxygen
isotopes (δ13C, δ18O)
of decade - old California mussel shells (Mytilus californianus) in the context
of an instrumental seawater
record of the same length.
The
record tells the story
of the sudden release
of an isotopically light source
of carbon, triggering a fast warming in the deep sea
of about 5 degrees C. Both the carbon
isotope signal and the temperature (inferred from oxygen
isotopes) then relaxed back toward their initial values in about 100,000 years.
Over even longer time scales (hundreds
of years) there are a number
of paleo -
records that correlate with
records of cosmogenic
isotopes (particularly 10Be and 14C), however, these
records are somewhat modulated by climate processes themselves (the carbon cycle in the case
of 14C, aerosol deposition and transport processes for 10Be) and so don't offer an absolutely clean attribution.
[Response: The ice core evidence regards the magnitude
of the eruption, not the climatic impact (though in principle, ice core
isotopes in some locations would
record the cooling signal).