Simon Blockley
Dados Biográficos
| ID | 1753092 |
|---|---|
| NOME | Simon Blockley |
| PRENOMES | Simon |
| SOBRENOME | Blockley |
| ASSINATURA | BLOCKLEY S |
| AFILIAÇÕES | Royal Holloway University of London |
| ORCID | 0000-0003-0712-2118 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 16 |
| TOTAL DE CITAÇÕES | 85 |
| TOTAL COMO AUTOR | 16 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2000 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2025 |
| ÍNDICE H | 4 |
Evidence from Tinshemet Cave in Israel suggests behavioural uniformity across Homo groups in the Levantine mid-Middle Palaeolithic circa 130,000-80,000 years ago
The south Levantine mid-Middle Palaeolithic (mid-MP; ~130-80 thousand years ago (ka)) is remarkable for its exceptional evidence of human morphological variability, with contemporaneous fossils of Homo sapiens and Neanderthal-like hominins. Yet, it remains unclear whether these hominins adhered to discrete behavioural sets or whether regional-scale intergroup interactions could have homogenized mid-MP behaviour. Here we report on our discoveries …
Holocene deglaciation and glacier readvances on the Fildes Peninsula and King George Island (Isla 25 de Mayo), South Shetland Islands, NW Antarctic Peninsula
To provide insights into glacier-climate dynamics of the South Shetland Islands (SSI), NW Antarctic Peninsula, we present a new deglaciation and readvance model for the Bellingshausen Ice Cap (BIC) on Fildes Peninsula and for King George Island/Isla 25 de Mayo (KGI) ~62°S. Deglaciation on KGI began after c. 15 cal. ka BP and had progressed to within present-day limits on the Fildes Peninsula, its largest ice-free peninsula, by c. 6.6–5.3 cal. ka …
Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3
Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during t…
Rare Holocene sediment deposits from Sodmein Playa (Eastern Desert, Egypt)—Stratigraphic assessment and environmental setting
Sodmein Playa is one of the rare Pleistocene open‐air sites in the Eastern Desert of Egypt. Based on the associated stone artefact material, it could be assigned to the Middle Stone Age/Last Interglacial. However, it has not yet been possible to clarify whether the sediments at the basin originated during the Pleistocene or later during Holocene wet phases. Our integrative approach combining Optically Stimulated Luminescence chronology, and crypt…
Scales of analysis
Early Levallois technology and the Lower to Middle Paleolithic transition in the Southern Caucasus
An early assemblage of obsidian artifacts Levallois technology is the name for the stone knapping technique used to create tools thousands of years ago. The technique appeared in the archeological record across Eurasia 200 to 300 thousand years ago (ka) and appeared earlier in Africa. Adler et al. challenge the hypothesis that the technique's appearance in Eurasia was the result of the expansion of hominins from Africa. Levallois obsidian artifac…
A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records
Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core records provide a master record of past climatic changes throughout the Last Interglacial–Glacial cycle in the North Atlantic region. As part of the INTIMATE (INTegration of Ice-core, MArine and TErrestrial records) project, protocols have been proposed to ensure consistent and robust correlation between different records of past climate. A key element of th…
Identification and correlation of visible tephras in the Lake Suigetsu SG06 sedimentary archive, Japan
Volcanic ash layers illuminate the resilience of Neanderthals and early modern humans to natural hazards
Marked changes in human dispersal and development during the Middle to Upper Paleolithic transition have been attributed to massive volcanic eruption and/or severe climatic deterioration. We test this concept using records of volcanic ash layers of the Campanian Ignimbrite eruption dated to ca. 40,000 y ago (40 ka B.P.). The distribution of the Campanian Ignimbrite has been enhanced by the discovery of cryptotephra deposits (volcanic ash layers t…
Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended Intimate event stratigraphy to 48,000 b2k
Developing distal tephrochronology for palaeoenvironmental reconstruction in Patagonia
Late Holocene vegetation and palaeoenvironmental history of the Dunadd area, Argyll, Scotland
Reevaluating the Age of the Iberomaurusian in Morocco
The Middle to Upper Paleolithic transition
Rapid human response to Late Glacial climate change
In their reply to our recent paper (Blockley et al.2000), Housley et ~ l(2.0 00) make four substantialpoints. Firstly, they assert that our critique oftheir two-stage re-colonization model rests solelyupon radiocarbon calibration. Secondly, and consequently,they point to problems with Late Glacialcalibration curves. Thirdly, they argue thatradiocarbon calibration should be advanced onlyfor sound archaeological reasons. Finally, theystate that our…
Radiocarbon calibration and Late Glacial occupation in northwest Europe
Various methods of analysing the dating of the late Glacial suggest various interpretations. Here, in answer to a paper from 1997, radiocarbon dates are calibrated and used to reconsider the dating of this contentious period
Reevaluating the Age of the Iberomaurusian in Morocco
The Middle to Upper Paleolithic transition
Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3
Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during t…
Radiocarbon calibration and Late Glacial occupation in northwest Europe
Various methods of analysing the dating of the late Glacial suggest various interpretations. Here, in answer to a paper from 1997, radiocarbon dates are calibrated and used to reconsider the dating of this contentious period
Rapid human response to Late Glacial climate change
In their reply to our recent paper (Blockley et al.2000), Housley et ~ l(2.0 00) make four substantialpoints. Firstly, they assert that our critique oftheir two-stage re-colonization model rests solelyupon radiocarbon calibration. Secondly, and consequently,they point to problems with Late Glacialcalibration curves. Thirdly, they argue thatradiocarbon calibration should be advanced onlyfor sound archaeological reasons. Finally, theystate that our…
Late Holocene vegetation and palaeoenvironmental history of the Dunadd area, Argyll, Scotland
Evidence from Tinshemet Cave in Israel suggests behavioural uniformity across Homo groups in the Levantine mid-Middle Palaeolithic circa 130,000-80,000 years ago
The south Levantine mid-Middle Palaeolithic (mid-MP; ~130-80 thousand years ago (ka)) is remarkable for its exceptional evidence of human morphological variability, with contemporaneous fossils of Homo sapiens and Neanderthal-like hominins. Yet, it remains unclear whether these hominins adhered to discrete behavioural sets or whether regional-scale intergroup interactions could have homogenized mid-MP behaviour. Here we report on our discoveries …
Scales of analysis
Rapid human response to Late Glacial climate change
In their reply to our recent paper (Blockley et al.2000), Housley et ~ l(2.0 00) make four substantialpoints. Firstly, they assert that our critique oftheir two-stage re-colonization model rests solelyupon radiocarbon calibration. Secondly, and consequently,they point to problems with Late Glacialcalibration curves. Thirdly, they argue thatradiocarbon calibration should be advanced onlyfor sound archaeological reasons. Finally, theystate that our…
Radiocarbon calibration and Late Glacial occupation in northwest Europe
Various methods of analysing the dating of the late Glacial suggest various interpretations. Here, in answer to a paper from 1997, radiocarbon dates are calibrated and used to reconsider the dating of this contentious period
Reevaluating the Age of the Iberomaurusian in Morocco
The Middle to Upper Paleolithic transition
Late Holocene vegetation and palaeoenvironmental history of the Dunadd area, Argyll, Scotland
Volcanic ash layers illuminate the resilience of Neanderthals and early modern humans to natural hazards
Marked changes in human dispersal and development during the Middle to Upper Paleolithic transition have been attributed to massive volcanic eruption and/or severe climatic deterioration. We test this concept using records of volcanic ash layers of the Campanian Ignimbrite eruption dated to ca. 40,000 y ago (40 ka B.P.). The distribution of the Campanian Ignimbrite has been enhanced by the discovery of cryptotephra deposits (volcanic ash layers t…
Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended Intimate event stratigraphy to 48,000 b2k
Developing distal tephrochronology for palaeoenvironmental reconstruction in Patagonia
Identification and correlation of visible tephras in the Lake Suigetsu SG06 sedimentary archive, Japan
Early Levallois technology and the Lower to Middle Paleolithic transition in the Southern Caucasus
An early assemblage of obsidian artifacts Levallois technology is the name for the stone knapping technique used to create tools thousands of years ago. The technique appeared in the archeological record across Eurasia 200 to 300 thousand years ago (ka) and appeared earlier in Africa. Adler et al. challenge the hypothesis that the technique's appearance in Eurasia was the result of the expansion of hominins from Africa. Levallois obsidian artifac…
A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records
Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core records provide a master record of past climatic changes throughout the Last Interglacial–Glacial cycle in the North Atlantic region. As part of the INTIMATE (INTegration of Ice-core, MArine and TErrestrial records) project, protocols have been proposed to ensure consistent and robust correlation between different records of past climate. A key element of th…
Scales of analysis
Rare Holocene sediment deposits from Sodmein Playa (Eastern Desert, Egypt)—Stratigraphic assessment and environmental setting
Sodmein Playa is one of the rare Pleistocene open‐air sites in the Eastern Desert of Egypt. Based on the associated stone artefact material, it could be assigned to the Middle Stone Age/Last Interglacial. However, it has not yet been possible to clarify whether the sediments at the basin originated during the Pleistocene or later during Holocene wet phases. Our integrative approach combining Optically Stimulated Luminescence chronology, and crypt…
Holocene deglaciation and glacier readvances on the Fildes Peninsula and King George Island (Isla 25 de Mayo), South Shetland Islands, NW Antarctic Peninsula
To provide insights into glacier-climate dynamics of the South Shetland Islands (SSI), NW Antarctic Peninsula, we present a new deglaciation and readvance model for the Bellingshausen Ice Cap (BIC) on Fildes Peninsula and for King George Island/Isla 25 de Mayo (KGI) ~62°S. Deglaciation on KGI began after c. 15 cal. ka BP and had progressed to within present-day limits on the Fildes Peninsula, its largest ice-free peninsula, by c. 6.6–5.3 cal. ka …
Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3
Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during t…
Evidence from Tinshemet Cave in Israel suggests behavioural uniformity across Homo groups in the Levantine mid-Middle Palaeolithic circa 130,000-80,000 years ago
The south Levantine mid-Middle Palaeolithic (mid-MP; ~130-80 thousand years ago (ka)) is remarkable for its exceptional evidence of human morphological variability, with contemporaneous fossils of Homo sapiens and Neanderthal-like hominins. Yet, it remains unclear whether these hominins adhered to discrete behavioural sets or whether regional-scale intergroup interactions could have homogenized mid-MP behaviour. Here we report on our discoveries …
Geography (13 obras) · Archaeology (12 obras) · Geology and Paleoclimatology Research (12 obras) · Pleistocene-Era Hominins and Archaeology (12 obras) · Archaeology and ancient environmental studies (11 obras) · Geology (9 obras) · Paleontology (9 obras) · Geology (8 obras) · Paleontology (8 obras) · Physical geography (8 obras)