Julian E Andrews
Biographic Data
| ID | 2776215 |
|---|---|
| NAME | Julian E Andrews |
| GIVEN NAMES | Julian E |
| FAMILY NAME | Andrews |
| SIGNATURE | ANDREWS J E |
| AFFILIATIONS | University of East Anglia |
| ORCID | 0000-0002-9843-0759 |
| VERIFIED | Yes |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 6 |
| AUTHOR COUNT | 7 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1994 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 2 |
Local-scale environmental gradients in ‘snail-shell’ stable isotopes from Holocene Jordanian archaeological sites
Reconstructing environments around archaeological sites is complicated by past land management practices and regional-scale climate proxies that can be contradictory and are often located at a distance from the sites themselves. Here we explore environmental information from fossil snail shells which, even when few in number on an archaeological site, may prove invaluable in constructing site-specific data. The palaeoecology of fossil snails and …
Professor Keith Clayton CBE
Professor Keith Clayton in 2003, 25 September 1928–12 February 2013 Source: Reproduced with kind permission of Eastern Daily Press In 1967 Professor Keith Clayton boldly accepted the challenge of setting up a School of Environmental Sciences at the fledgling University of East Anglia (UEA) in Norwich, a concept of Lord Solly Zuckerman. As a reader in Geography at the London School of Economics (LSE) Keith Clayton could surely have pursued a simpl…
Saints and Sinners: A tephrochronology for Late Antique landscape change in Epirus from the eruptive history of Lipari, Aeolian Islands
Nutrient Fluxes Through the Humber Estuary—Past, Present and Future
The geomorphology of the present day and Holocene (3000 years ago) Humber estuary, United Kingdom, are described. More than 90% of the intertidal area and sediment accumulation capacity of the estuary has been lost to reclamation over this period. A similar situation prevails in many other urbanized estuaries. Nutrient budgets for the modern estuary are presented demonstrating little trapping of nutrients, due to the loss of intertidal areas. A s…
Nutrient Fluxes Through the Humber Estuary—Past, Present and Future
The geomorphology of the present day and Holocene (3000 years ago) Humber estuary, United Kingdom, are described. More than 90% of the intertidal area and sediment accumulation capacity of the estuary has been lost to reclamation over this period. A similar situation prevails in many other urbanized estuaries. Nutrient budgets for the modern estuary are presented demonstrating little trapping of nutrients, due to the loss of intertidal areas. A s…
Do Stable Isotope Data from Calcrete Record Late Pleistocene Monsoonal Climate Variation in the Thar Desert of India?
Late Pleistocene terrestrial climate records in India may be preserved in oxygen and carbon stable isotopes in pedogenic calcrete. Petrography shows that calcrete nodules in Quaternary sediments of the Thar Desert in Rajasthan are pedogenic, with little evidence for postpedogenic alteration. The calcrete occurs in four laterally persistent and one nonpersistent eolian units, separated by colluvial gravel. Thermoluminescence and infrared- and gree…
Stable isotope record of palaeoclimatic change in a British Holocene tufa
A 9.5 m long, continuous core through Holocene tufa deposits in Derbyshire, UK, was analysed for oxygen and carbon stable isotope variations with a view to palaeoclimatic and palaeoenvir onmental interpretation. The depositional environment of the tufa is well understood and dated using 14 C and biostratigraphy. It is argued that smooth variations of up to 1‰ in δ 18 O of the tufa calcites are caused by changes in the isotopic composition of regi…
Stable isotope record of palaeoclimatic change in a British Holocene tufa
A 9.5 m long, continuous core through Holocene tufa deposits in Derbyshire, UK, was analysed for oxygen and carbon stable isotope variations with a view to palaeoclimatic and palaeoenvir onmental interpretation. The depositional environment of the tufa is well understood and dated using 14 C and biostratigraphy. It is argued that smooth variations of up to 1‰ in δ 18 O of the tufa calcites are caused by changes in the isotopic composition of regi…
Saints and Sinners: A tephrochronology for Late Antique landscape change in Epirus from the eruptive history of Lipari, Aeolian Islands
Local-scale environmental gradients in ‘snail-shell’ stable isotopes from Holocene Jordanian archaeological sites
Reconstructing environments around archaeological sites is complicated by past land management practices and regional-scale climate proxies that can be contradictory and are often located at a distance from the sites themselves. Here we explore environmental information from fossil snail shells which, even when few in number on an archaeological site, may prove invaluable in constructing site-specific data. The palaeoecology of fossil snails and …
Stable isotope record of palaeoclimatic change in a British Holocene tufa
A 9.5 m long, continuous core through Holocene tufa deposits in Derbyshire, UK, was analysed for oxygen and carbon stable isotope variations with a view to palaeoclimatic and palaeoenvir onmental interpretation. The depositional environment of the tufa is well understood and dated using 14 C and biostratigraphy. It is argued that smooth variations of up to 1‰ in δ 18 O of the tufa calcites are caused by changes in the isotopic composition of regi…
Do Stable Isotope Data from Calcrete Record Late Pleistocene Monsoonal Climate Variation in the Thar Desert of India?
Late Pleistocene terrestrial climate records in India may be preserved in oxygen and carbon stable isotopes in pedogenic calcrete. Petrography shows that calcrete nodules in Quaternary sediments of the Thar Desert in Rajasthan are pedogenic, with little evidence for postpedogenic alteration. The calcrete occurs in four laterally persistent and one nonpersistent eolian units, separated by colluvial gravel. Thermoluminescence and infrared- and gree…
Nutrient Fluxes Through the Humber Estuary—Past, Present and Future
The geomorphology of the present day and Holocene (3000 years ago) Humber estuary, United Kingdom, are described. More than 90% of the intertidal area and sediment accumulation capacity of the estuary has been lost to reclamation over this period. A similar situation prevails in many other urbanized estuaries. Nutrient budgets for the modern estuary are presented demonstrating little trapping of nutrients, due to the loss of intertidal areas. A s…
Nutrient Fluxes Through the Humber Estuary—Past, Present and Future
The geomorphology of the present day and Holocene (3000 years ago) Humber estuary, United Kingdom, are described. More than 90% of the intertidal area and sediment accumulation capacity of the estuary has been lost to reclamation over this period. A similar situation prevails in many other urbanized estuaries. Nutrient budgets for the modern estuary are presented demonstrating little trapping of nutrients, due to the loss of intertidal areas. A s…
Saints and Sinners: A tephrochronology for Late Antique landscape change in Epirus from the eruptive history of Lipari, Aeolian Islands
Professor Keith Clayton CBE
Professor Keith Clayton in 2003, 25 September 1928–12 February 2013 Source: Reproduced with kind permission of Eastern Daily Press In 1967 Professor Keith Clayton boldly accepted the challenge of setting up a School of Environmental Sciences at the fledgling University of East Anglia (UEA) in Norwich, a concept of Lord Solly Zuckerman. As a reader in Geography at the London School of Economics (LSE) Keith Clayton could surely have pursued a simpl…
Local-scale environmental gradients in ‘snail-shell’ stable isotopes from Holocene Jordanian archaeological sites
Reconstructing environments around archaeological sites is complicated by past land management practices and regional-scale climate proxies that can be contradictory and are often located at a distance from the sites themselves. Here we explore environmental information from fossil snail shells which, even when few in number on an archaeological site, may prove invaluable in constructing site-specific data. The palaeoecology of fossil snails and …
Geography (5 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Archaeology (3 works) · Biology (3 works) · Ecology (3 works) · Geology (3 works) · Oceanography (3 works) · Oceanography (3 works) · Paleontology (3 works)