Marc W Caffee

Datos Biográficos

ID	4129635
NOMBRE	Marc W Caffee
NOMBRES	Marc W
APELLIDO	Caffee
FIRMA	CAFFEE M W
AFILIACIONES	Purdue University West Lafayette
ORCID	0000-0002-6846-8967
VERIFICADO	Sí
TOTAL DE OBRAS	18
TOTAL DE CITAS	0
TOTAL COMO AUTOR	18
TOTAL COMO EDITOR	0
PRIMER AÑO DE PUBLICACIÓN	2001
AÑO MÁS RECIENTE DE PUBLICACIÓN	2024
ÍNDICE H	0

Be surface exposure dating of glacier fluctuations on the eastern slope of Mount Geladandong, central Tibetan Plateau
Open AccessJingdong Zhao, Jinkun Qiu et al.ARTICLEQuaternary International2024
Timing and extent of Late Pleistocene glaciation in the Chugach Mountains, Alaska
Open AccessJoshua D Valentino, Joshua Valentino et al.ARTICLEQuaternary Research2021
Geomorphic mapping, landform and sediment analysis, and cosmogenic 10 Be and 36 Cl ages from erratics, moraine boulders, and glacially polished bedrock help define the timing of the Wisconsinan glaciations in the Chugach Mountains of south-central Alaska. The maximum extent of glaciation in the Chugach Mountains during the last glacial period (marine isotope stages [MIS] 5d through 2) occurred at ~50 ka during MIS 3. In the Williwaw Lakes valley …
Climate during the Last Glacial Maximum in the Northern Sawatch Range, Colorado, USA
Open AccessKeith A Brugger, Chester A Ruleman et al.ARTICLEQuaternary2019
Temperature-index modeling is used to determine the magnitude of temperature depression in the northern Sawatch Range required to maintain steady-state mass balances of six reconstructed glaciers at their extent during the local Last Glacial Maximum (LLGM), dated at ~21 ka. Assuming no significant differences in precipitation compared to modern values, mean annual temperatures in the region were on average 8.8 + 0.5/– 0.8 °C cooler than they are …
Cosmogenic nuclide age estimate for Laurentide Ice Sheet recession from the terminal moraine, New Jersey, USA, and constraints on latest Pleistocene ice sheet history
Open AccessLee B Corbett, Paul R Bierman et al.ARTICLEQuaternary Research2017
The time at which the Laurentide Ice Sheet reached its maximum extent and subsequently retreated from its terminal moraine in New Jersey has been constrained by bracketing radiocarbon ages on preglacial and postglacial sediments. Here, we present measurements of in situ produced 10 Be and 26 Al in 16 quartz-bearing samples collected from bedrock outcrops and glacial erratics just north of the terminal moraine in north-central New Jersey; as such,…
Deglaciation of Fennoscandia
Open AccessArjen P Stroeven, Clas Hättestrand et al.ARTICLEQuaternary Science Reviews2016
To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and geochronological data from radiocarbon, varve, optically-stimulated luminescence, and cosmogenic…
Timing and climate forcing of volcanic eruptions for the past 2,500 years
Open AccessMichael Sigl, Mai Winstrup et al.ARTICLENature2015
New cosmogenic burial ages for Sterkfontein Member 2 Australopithecus and Member 5 Oldowan
Open AccessDarryl E Granger, Ryan J Gibbon et al.ARTICLENature2015
Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan, northeastern Tibetan Plateau
Open AccessJie Wang, Christine Kassab et al.ARTICLEQuaternary Research2013
Cosmogenic nuclide (CN) apparent exposure dating has become a widely used method for determining the age of glacial landforms on the Tibetan Plateau with > 1200 published ages. We present the first 10 Be exposure ages from the Dalijia Shan, the most northeastern formerly glaciated mountain range on the Tibetan Plateau. The moraine groups identified from field and remote sensing imagery mapping record four glacial events at 37.07 ± 3.70 to 52.96 ±…
Importance of sampling across an assemblage of glacial landforms for interpreting cosmogenic ages of deglaciation
Open AccessArjen P Stroeven, Derek Fabel et al.ARTICLEQuaternary Research2011
Deglaciation chronologies for some sectors of former ice sheets are relatively poorly constrained because of the paucity of features or materials traditionally used to constrain the timing of deglaciation. In areas without good deglaciation varve chronologies and/or without widespread occurrence of material that indicates the start of earliest organic radiocarbon accumulations suitable for radiocarbon dating, typically only general patterns and c…
Late Quaternary glacial chronology on Nevado Illimani, Bolivia, and the implications for paleoclimatic reconstructions across the Andes
Open AccessColby A Smith, Thomas V Lowell et al.ARTICLEQuaternary Research2011
10 Be terrestrial cosmogenic nuclide surface exposure ages from moraines on Nevado Illimani, Cordillera Real, Bolivia suggest that glaciers retreated from moraines during the periods 15.5–13.0 ka, 10.0–8.5 ka, and 3.5–2.0 ka. Late glacial moraines at Illimani are associated with an ELA depression of 400–600 m, which is consistent with other local reconstructions of late glacial ELAs in the Eastern Cordillera of the central Andes. A comparison of …
The role of mass movements on landscape evolution in the Central Karakoram
Open AccessJohn F Shroder, Lewis A Owen et al.ARTICLEQuaternary International2011
Towards defining the transition in style and timing of Quaternary glaciation between the monsoon-influenced Greater Himalaya and the semi-arid Transhimalaya of Northern India
Open AccessKathryn A Hedrick, Yeong Bae Seong et al.ARTICLEQuaternary International2011
Quaternary glaciation in the Nubra and Shyok valley confluence, northernmost Ladakh, India
Open AccessJason M Dortch, Lewis A Owens et al.ARTICLEQuaternary Research2010
Three glacial stages (Deshkit 1, Deshkit 2 and Dishkit 3 glacial stages) are identified in the Nubra and Shyok valleys in northernmost Ladakh, northwest India, on the basis of geomorphic field mapping, remote sensing, and 10 Be terrestrial cosmogenic nuclide surface exposure dating. The glacial stages date to ∼ 45 ka (Deshkit 1 glacial stage), ∼ 81 ka (Deshkit 2 glacial stage) and ∼ 144 ka (Deshkit 3 glacial stage). A mean equilibrium line altitu…
Last glacial maximum climate inferences from cosmogenic dating and glacier modeling of the western Uinta ice field, Uinta Mountains, Utah
Open AccessKurt A Refsnider, Benjamin Laabs et al.ARTICLEQuaternary Research2008
During the last glacial maximum (LGM), the western Uinta Mountains of northeastern Utah were occupied by the Western Uinta Ice Field. Cosmogenic 10 Be surface-exposure ages from the terminal moraine in the North Fork Provo Valley and paired 26 Al and 10 Be ages from striated bedrock at Bald Mountain Pass set limits on the timing of the local LGM. Moraine boulder ages suggest that ice reached its maximum extent by 17.4±0.5 ka (± 2σ). 10 Be and 26 …
Timing of surficial process changes down a Mojave Desert piedmont
Open AccessKyle K Nichols, Paul R Bierman et al.ARTICLEQuaternary Research2007
We measured 10 Be and 26 Al in 29 sediment samples to infer the history and millennial-scale rates of change down a low-gradient piedmont, a common but enigmatic landform that dominates the Mojave Desert. Nuclide data suggest that a large volume of sediment was deposited on the proximal East Range Road piedmont in Fort Irwin, California, ∼ 75,500 yr ago. Since then, this material has been stable or eroding slowly. In contrast, on the distal piedm…
Cosmogenic nuclide chronology of pre-last glacial maximum moraines at Lago Buenos Aires, 46 S, Argentina
Open AccessMichael R Kaplan, Daniel C Douglass et al.ARTICLEQuaternary Research2005
At Lago Buenos Aires, Argentina, 10 Be, 26 Al, and 40 Ar/ 39 Ar ages range from 190,000 to 109,000 yr for two moraines deposited prior to the last glaciation, 23,000 16,000 yr ago. Two approaches, maximum boulder ages assuming no erosion, and the average age of all boulders and an erosion rate of 1.4 mm/10 3 yr, both yield a common estimate age of 150,000 140,000 yr for the two moraines. The erosion rate estimate derives from 10 Be and 26 Al conc…
Lower Pliocene Hominid Remains from Sterkfontein
Open AccessT C Partridge, Darryl E Granger et al.ARTICLEScience2003
Cosmogenic aluminum-26 and beryllium-10 burial dates of low-lying fossiliferous breccia in the caves at Sterkfontein, South Africa, show that associated hominid fossils accumulated in the Lower Pliocene. These dates indicate that the skeleton StW 573 and newly discovered specimens from Jacovec Cavern have much the same age: approximately 4 million years. These specimens are thus of an age similar to Australopithecus anamensis from East Africa.
Late Pleistocene Cosmogenic 36 Cl Glacial Chronology of the Southwestern Ahklun Mountains, Alaska
Open AccessJason P Briner, Terry W Swanson et al.ARTICLEQuaternary Research2001
Thirty-two cosmogenic 36 Cl surface exposure ages constrain the timing of two late Pleistocene glacial advances in the western Ahklun Mountains, southwestern Alaska. Boulders were sampled from one early Wisconsin ( sensu lato ) and six late Wisconsin moraines deposited by ice-cap outlet glaciers and local alpine glaciers. Four moraine boulders deposited during an extensive early Wisconsin ice-cap outlet glacier advance have a mean surface exposur…

Late Pleistocene Cosmogenic 36 Cl Glacial Chronology of the Southwestern Ahklun Mountains, Alaska
Open AccessJason P Briner, Terry W Swanson et al.ARTICLEQuaternary Research2001
Thirty-two cosmogenic 36 Cl surface exposure ages constrain the timing of two late Pleistocene glacial advances in the western Ahklun Mountains, southwestern Alaska. Boulders were sampled from one early Wisconsin ( sensu lato ) and six late Wisconsin moraines deposited by ice-cap outlet glaciers and local alpine glaciers. Four moraine boulders deposited during an extensive early Wisconsin ice-cap outlet glacier advance have a mean surface exposur…
Lower Pliocene Hominid Remains from Sterkfontein
Open AccessT C Partridge, Darryl E Granger et al.ARTICLEScience2003
Cosmogenic aluminum-26 and beryllium-10 burial dates of low-lying fossiliferous breccia in the caves at Sterkfontein, South Africa, show that associated hominid fossils accumulated in the Lower Pliocene. These dates indicate that the skeleton StW 573 and newly discovered specimens from Jacovec Cavern have much the same age: approximately 4 million years. These specimens are thus of an age similar to Australopithecus anamensis from East Africa.
Cosmogenic nuclide chronology of pre-last glacial maximum moraines at Lago Buenos Aires, 46 S, Argentina
Open AccessMichael R Kaplan, Daniel C Douglass et al.ARTICLEQuaternary Research2005
At Lago Buenos Aires, Argentina, 10 Be, 26 Al, and 40 Ar/ 39 Ar ages range from 190,000 to 109,000 yr for two moraines deposited prior to the last glaciation, 23,000 16,000 yr ago. Two approaches, maximum boulder ages assuming no erosion, and the average age of all boulders and an erosion rate of 1.4 mm/10 3 yr, both yield a common estimate age of 150,000 140,000 yr for the two moraines. The erosion rate estimate derives from 10 Be and 26 Al conc…
Timing of surficial process changes down a Mojave Desert piedmont
Open AccessKyle K Nichols, Paul R Bierman et al.ARTICLEQuaternary Research2007
We measured 10 Be and 26 Al in 29 sediment samples to infer the history and millennial-scale rates of change down a low-gradient piedmont, a common but enigmatic landform that dominates the Mojave Desert. Nuclide data suggest that a large volume of sediment was deposited on the proximal East Range Road piedmont in Fort Irwin, California, ∼ 75,500 yr ago. Since then, this material has been stable or eroding slowly. In contrast, on the distal piedm…
Last glacial maximum climate inferences from cosmogenic dating and glacier modeling of the western Uinta ice field, Uinta Mountains, Utah
Open AccessKurt A Refsnider, Benjamin Laabs et al.ARTICLEQuaternary Research2008
During the last glacial maximum (LGM), the western Uinta Mountains of northeastern Utah were occupied by the Western Uinta Ice Field. Cosmogenic 10 Be surface-exposure ages from the terminal moraine in the North Fork Provo Valley and paired 26 Al and 10 Be ages from striated bedrock at Bald Mountain Pass set limits on the timing of the local LGM. Moraine boulder ages suggest that ice reached its maximum extent by 17.4±0.5 ka (± 2σ). 10 Be and 26 …
Quaternary glaciation in the Nubra and Shyok valley confluence, northernmost Ladakh, India
Open AccessJason M Dortch, Lewis A Owens et al.ARTICLEQuaternary Research2010
Three glacial stages (Deshkit 1, Deshkit 2 and Dishkit 3 glacial stages) are identified in the Nubra and Shyok valleys in northernmost Ladakh, northwest India, on the basis of geomorphic field mapping, remote sensing, and 10 Be terrestrial cosmogenic nuclide surface exposure dating. The glacial stages date to ∼ 45 ka (Deshkit 1 glacial stage), ∼ 81 ka (Deshkit 2 glacial stage) and ∼ 144 ka (Deshkit 3 glacial stage). A mean equilibrium line altitu…
Importance of sampling across an assemblage of glacial landforms for interpreting cosmogenic ages of deglaciation
Open AccessArjen P Stroeven, Derek Fabel et al.ARTICLEQuaternary Research2011
Deglaciation chronologies for some sectors of former ice sheets are relatively poorly constrained because of the paucity of features or materials traditionally used to constrain the timing of deglaciation. In areas without good deglaciation varve chronologies and/or without widespread occurrence of material that indicates the start of earliest organic radiocarbon accumulations suitable for radiocarbon dating, typically only general patterns and c…
Late Quaternary glacial chronology on Nevado Illimani, Bolivia, and the implications for paleoclimatic reconstructions across the Andes
Open AccessColby A Smith, Thomas V Lowell et al.ARTICLEQuaternary Research2011
10 Be terrestrial cosmogenic nuclide surface exposure ages from moraines on Nevado Illimani, Cordillera Real, Bolivia suggest that glaciers retreated from moraines during the periods 15.5–13.0 ka, 10.0–8.5 ka, and 3.5–2.0 ka. Late glacial moraines at Illimani are associated with an ELA depression of 400–600 m, which is consistent with other local reconstructions of late glacial ELAs in the Eastern Cordillera of the central Andes. A comparison of …
The role of mass movements on landscape evolution in the Central Karakoram
Open AccessJohn F Shroder, Lewis A Owen et al.ARTICLEQuaternary International2011
Towards defining the transition in style and timing of Quaternary glaciation between the monsoon-influenced Greater Himalaya and the semi-arid Transhimalaya of Northern India
Open AccessKathryn A Hedrick, Yeong Bae Seong et al.ARTICLEQuaternary International2011
Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan, northeastern Tibetan Plateau
Open AccessJie Wang, Christine Kassab et al.ARTICLEQuaternary Research2013
Cosmogenic nuclide (CN) apparent exposure dating has become a widely used method for determining the age of glacial landforms on the Tibetan Plateau with > 1200 published ages. We present the first 10 Be exposure ages from the Dalijia Shan, the most northeastern formerly glaciated mountain range on the Tibetan Plateau. The moraine groups identified from field and remote sensing imagery mapping record four glacial events at 37.07 ± 3.70 to 52.96 ±…
Timing and climate forcing of volcanic eruptions for the past 2,500 years
Open AccessMichael Sigl, Mai Winstrup et al.ARTICLENature2015
New cosmogenic burial ages for Sterkfontein Member 2 Australopithecus and Member 5 Oldowan
Open AccessDarryl E Granger, Ryan J Gibbon et al.ARTICLENature2015
Deglaciation of Fennoscandia
Open AccessArjen P Stroeven, Clas Hättestrand et al.ARTICLEQuaternary Science Reviews2016
To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and geochronological data from radiocarbon, varve, optically-stimulated luminescence, and cosmogenic…
Cosmogenic nuclide age estimate for Laurentide Ice Sheet recession from the terminal moraine, New Jersey, USA, and constraints on latest Pleistocene ice sheet history
Open AccessLee B Corbett, Paul R Bierman et al.ARTICLEQuaternary Research2017
The time at which the Laurentide Ice Sheet reached its maximum extent and subsequently retreated from its terminal moraine in New Jersey has been constrained by bracketing radiocarbon ages on preglacial and postglacial sediments. Here, we present measurements of in situ produced 10 Be and 26 Al in 16 quartz-bearing samples collected from bedrock outcrops and glacial erratics just north of the terminal moraine in north-central New Jersey; as such,…
Climate during the Last Glacial Maximum in the Northern Sawatch Range, Colorado, USA
Open AccessKeith A Brugger, Chester A Ruleman et al.ARTICLEQuaternary2019
Temperature-index modeling is used to determine the magnitude of temperature depression in the northern Sawatch Range required to maintain steady-state mass balances of six reconstructed glaciers at their extent during the local Last Glacial Maximum (LLGM), dated at ~21 ka. Assuming no significant differences in precipitation compared to modern values, mean annual temperatures in the region were on average 8.8 + 0.5/– 0.8 °C cooler than they are …
Timing and extent of Late Pleistocene glaciation in the Chugach Mountains, Alaska
Open AccessJoshua D Valentino, Joshua Valentino et al.ARTICLEQuaternary Research2021
Geomorphic mapping, landform and sediment analysis, and cosmogenic 10 Be and 36 Cl ages from erratics, moraine boulders, and glacially polished bedrock help define the timing of the Wisconsinan glaciations in the Chugach Mountains of south-central Alaska. The maximum extent of glaciation in the Chugach Mountains during the last glacial period (marine isotope stages [MIS] 5d through 2) occurred at ~50 ka during MIS 3. In the Williwaw Lakes valley …
Be surface exposure dating of glacier fluctuations on the eastern slope of Mount Geladandong, central Tibetan Plateau
Open AccessJingdong Zhao, Jinkun Qiu et al.ARTICLEQuaternary International2024