Late Quaternary (24-10 ka BP) environmental history of the Neotropical lowlands inferred from ostracodes in sediments of Lago Petén Itzá, Guatemala

Keyphrases

• Guatemala 100%
• Environmental History 100%
• Lowland 100%
• Ostracodes 100%
• Last Glacial Maximum 37%
• Core Sites 37%
• Deglacial 37%
• Early Holocene 25%
• Species Richness 25%
• Drying Conditions 25%
• CN Ratio 25%
• Water Depth 25%
• Nektobenthic 25%
• Central America 12%
• Sediment Core 12%
• Water Level 12%
• Aquatic Ecosystems 12%
• Environmental Conditions 12%
• Late Pleistocene 12%
• Peninsula 12%
• Gypsum 12%
• Transfer Function 12%
• Precipitation Gradient 12%
• Multivariate Statistics 12%
• Lake Sediments 12%
• Total Organic Carbon 12%
• Clayey Sediments 12%
• Wet Condition 12%
• Shallow Water 12%
• Lake Depth 12%
• Littoral Zone 12%
• Altitudinal Range 12%
• Water Zone 12%
• Punctata 12%
• Pleistocene Sediments 12%
• Shallow Littoral 12%
• Late Pleistocene-Holocene 12%
• Early Holocene Climate 12%
• Strandesia 12%
• Cytheridella 12%

Earth and Planetary Sciences

• Guatemala 100%
• Ostracod 100%
• Environmental History 100%
• Last Glacial Maximum 37%
• Early Holocene 37%
• Late Pleistocene 25%
• Water Depth 25%
• Species Richness 25%
• Holocene 12%
• Central America 12%
• Sediment Core 12%
• Lacustrine Deposit 12%
• Peninsula 12%
• Shallow Water 12%
• Multivariate Analysis 12%
• Intertidal Zone 12%
• Deep Water 12%
• Aquatic Environment 12%
• Organic Carbon 12%
• Transfer Function 12%