EXTRACT (SEE PDF FOR FULL ABSTRACT): The Holocene history of flooding in northern coastal Peru is believed to be a proxy record for the El Niño phenomenon. A recently completed set of 30 radiocarbon dates on overbank flood deposits and a tsunami deposit from the Casma region (Figure 1 and Table 1) establishes a chronology for the largest events that have occurred during the last 3500 years. ... The data presented here indicate that events much larger than the one in 1982-1983 may occur with a frequency of about once every 1000 years
International audienceThe La Tolita archeological site is located in the Province of Esmeraldas in t...
Data about the magnitude and time of occurrence of palaeofloods from the lower Colorado River basin ...
The Late Archaic Period (2600–1600 BC) site of Caral, located ~20 km inland from the Pacific Ocean c...
Here we present a high-resolution marine sediment record from the El Niño region off the coast of Pe...
The entire coast of Perú was surveyed to document deposits of historical tsunami. Evidence of four t...
Abstract It has previously been hypothesized that the sequences of beach ridges observed at the mout...
Analyzing the long-term behavior of the coastlines in the vicinity of river mouths and estuaries usu...
The El Nino global climate anomaly is a major cause of weather variation that can have far-reaching ...
In the general absence of standard, high-resolution paleoclimatic records such as lake cores or cora...
From the 18th International Radiocarbon Conference held in Wellington, New Zealand, September 1-5, 2...
Through an extensive sampling and dating of pairs of associated shells and charcoal fragments combin...
Field research conducted since the year 2000 in southern Europe (Portugal, Spain, Greece, Cyprus and...
The Pacific Ocean is a dominant driver of global climate variability on interannual to multidecadal ...
Through an extensive sampling and dating of pairs of associated shells and charcoal fragments combin...
The purpose of this research is to characterize Peruvian upwelling during the late Holocene (last 20...
International audienceThe La Tolita archeological site is located in the Province of Esmeraldas in t...
Data about the magnitude and time of occurrence of palaeofloods from the lower Colorado River basin ...
The Late Archaic Period (2600–1600 BC) site of Caral, located ~20 km inland from the Pacific Ocean c...
Here we present a high-resolution marine sediment record from the El Niño region off the coast of Pe...
The entire coast of Perú was surveyed to document deposits of historical tsunami. Evidence of four t...
Abstract It has previously been hypothesized that the sequences of beach ridges observed at the mout...
Analyzing the long-term behavior of the coastlines in the vicinity of river mouths and estuaries usu...
The El Nino global climate anomaly is a major cause of weather variation that can have far-reaching ...
In the general absence of standard, high-resolution paleoclimatic records such as lake cores or cora...
From the 18th International Radiocarbon Conference held in Wellington, New Zealand, September 1-5, 2...
Through an extensive sampling and dating of pairs of associated shells and charcoal fragments combin...
Field research conducted since the year 2000 in southern Europe (Portugal, Spain, Greece, Cyprus and...
The Pacific Ocean is a dominant driver of global climate variability on interannual to multidecadal ...
Through an extensive sampling and dating of pairs of associated shells and charcoal fragments combin...
The purpose of this research is to characterize Peruvian upwelling during the late Holocene (last 20...
International audienceThe La Tolita archeological site is located in the Province of Esmeraldas in t...
Data about the magnitude and time of occurrence of palaeofloods from the lower Colorado River basin ...
The Late Archaic Period (2600–1600 BC) site of Caral, located ~20 km inland from the Pacific Ocean c...